day 2 part 2 Flashcards

1
Q

proposes ores are direct magmatic product or are formed as products of differentiation

A

plutonism (magmatists)

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2
Q

proposes that ore deposits were formed from sediments in a primeval ocean

A

neptunism (syngenetic ore)

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3
Q

ore formed as the same time as the host rock

A

syngenetic ore

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4
Q

ore formed after the formation of the host rock

A

epigenetic ore

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5
Q

ore formed within the Earth

A

hypogene ore

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6
Q

ore formed at the surface or near the surface of the Earth

A

supergene ore

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7
Q

ore formed from either magmas or fluids

A

primary ore

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8
Q

ore formed due to the alteration of pre existing rocks or minerals

A

secondary ore

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9
Q

rock loving mineral

A

lithophile

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10
Q

iron loving mineral

A

siderophile

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11
Q

ore loving mineral

A

chalcophile

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12
Q

gas loving mineral

A

atmophile

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13
Q

cinnabar and hematite were used by early humans as pigments and used as gemstones and native Au Ag Cu as ornaments

A

Pre historic times

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14
Q

paleolithic man used various minerals as tints for paints

A

400,000 BCE stone age era

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15
Q

neolithic man became familiar and acquainted with gold and copper

A

new stone age

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16
Q

clay became the first larger scale mineral in the history of the mining industry

A

30,000-20,000 BCE

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17
Q

estimated date of discovery for copper and gold was used before its discovery

A

18,000 BCE

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18
Q

utilized clays as buildings materials

A

babylonians and early egyptian times

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19
Q

made pyramids using limestones
sank shafts at the coast of Red Sea in seach of emeralds

A

Egyptian times

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20
Q

gemstone mining reached a high value for art among Egyptians, Babylonians, Assyrians and Indians

A

~3400 BCE

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21
Q

mesopotamians developed bronce by replacing little amounts of tin to higher amounts of copper instead of using arsenic

A

2,500 BCE bronze age

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22
Q

first noted the occurrence of gold in quartz veins by herodotus

A

484-425 BCE

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23
Q

16 minerals grouped as metals stones and earth were described by theophratus a pupil of aristotle

A

372-287 BCE

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24
Q

avicenna grouped minerals as stones sulfur minerals metals and salts first noting sulfide group of minerals

A

980-1037 CE dark ages

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25
Q

agricola father of economic geol wrote the first publication for mining de re merallica libri XII which noted the process for fissure filling smelting and classification of ore deposits

A

1494-1555

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26
Q

steno proposed ores as products of condesation from vapors ascending through fissures

A

1669

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27
Q

henkel and zimmerman noted the importance of hydrothermal solutions and vapors of deep seated origin

A

1725-1746

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28
Q

van oppel distinguished discordant veins from concordant bedded deposits

A

1749

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29
Q

charpenteir noted metals and minerals in the veins were the resul of alteration reactions between country rock and water that had passed through them

A

1778-1799

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30
Q

integration of chemical concepts with ore genesis began
mining methods were improved allowing bigger and deeper mines to develop

A

19th century

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31
Q

waldemar lindgreen stated that pyrometasomatic deposits high temp replacemetns bodies near the borded zones of igneous intrusions and classified hydrothermal deposits into hypothermal mesothermal epithermal

A

1860-1939

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32
Q

classification of ore deposits evolved from P-T conditions to modes of occurrence

A

20th century

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33
Q

RAF penrose founded society of economic geology

A

1905

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34
Q

henry hoover and lou henry hoover published the English translation of de re metallica libri XII

A

1912

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35
Q

almost complete relinquishment of lindgreens ore classification

A

1960-70s

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36
Q

high temperature alteration resulting in potassium enrichment and abundance of biotite k feldspar and adularia

A

potassic

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37
Q

alteration that turns rocks green from the formation of chlorite epidote and actinolite

A

propylitic

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38
Q

replacement or decomposition of feldspar into sericite that implies acidic conditions

A

sericitic

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39
Q

low temperature alteration resulting in bleaching out of feldspars and intro of clay minerals

A

argillic

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40
Q

highly acidic alteration resulting in leaching and alteration of feldspar to seircite and assemblage formation of kaolinite + quartz + hematite + limonite

A

advanced argillic

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41
Q

most common alteration with the addition of secondary silica and formation of chalcedony

A

silicification

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42
Q

addition of any silicate mineral that forms in association with quartz typically biotite garnet or tourmaline

A

silication

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43
Q

form of silication that forms greissen with quartz muscovite and topaz with tourmaline fluorite rutile cassiterite adn wolframite

A

greisenization

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44
Q

alteration forming Ca- and Mg silicates

A

Skarn

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45
Q

relatively high temp alteration with Na enrichment and forms albite or sodic plag with possible paragonite

A

albitic

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46
Q

alteration of Ca plag into saussurite: zoisite + chlorite + amphibole + carbonates

A

saussuritization

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47
Q

last stage replacement process of uralitic amphibole into primary pyroxene and pyroxene to amphibole

A

uralitization

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48
Q

alteration resulting of addition of carbonates with talc chlorite sericite and albite

A

carbonization

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49
Q

alteration associated with alunite and hot springs environment implying presence of high SO4 gas

A

alunitic

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50
Q

low temp alteration forming zeolite minerals often associated with volcanic environments at a distance during its waning stages

A

zeolitic

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51
Q

low temperature alteration of mafic to ultramafic rocks into serpentine minerals that may occur with talc if there is a high concentration of Mg

A

serpentinization

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52
Q

alteration with variable temperature range and forms any type of oxide mineral

A

oxidation

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53
Q

localizes deposits lighter than the magma

A

structure highs

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54
Q

accumulates deposits heavier than melt at the bottom intrusives

A

structural lows

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55
Q

provides pathways for solutions to deposit

A

folds

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56
Q

controls deposition of ore deposits

A

fractures/lineaments

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57
Q

increases permeability where different fluids can interact and deposit ore

A

intersections

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58
Q

localizes or disperses deposits in fractures

A

faults

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59
Q

controls ore fluids before deposition

A

syngenetic

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60
Q

cut and displaces ore bodies

A

epigenetic

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61
Q

high velocity volcanic explosion vent where volcanic material are brought up rapidly

A

diatremes

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62
Q

solutions from different sources which carries metals for precipitation

A

ore bearing fluids

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63
Q

high temp rock melt of liquid and crystals with an inhomogeneous composition due to fractions and can cause ore formation due to metallic concentration

A

magma/magmatic fluids

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64
Q

mafic proportions :
silicic proportions:

A

Cr Ni Pt P
Sn Th Zr

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65
Q

oxide or sulfide dominated magma that solidify directly as ore

A

ore magma

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66
Q

oxide or sulfide dominated magma that solidify directly as ore

A

ore magma

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67
Q

aqueous high temp ore bearing fluid solution 100-800C

A

hydrothermal fluids

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68
Q

water at critical temp 376C that steadily becomes less dense without boiling

A

supercritical fluid

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69
Q

fractionated fluids and volatiles that travel upward from the magma that exsolves as an emulsion of water droplets attracting hydrophilic elements or ions

A

magmatic/juvenile waters

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70
Q

fossil waters

A

connate waters

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71
Q

chemical replacement of minerals where hydrothermal fluids deliver chemical reactants that removes aqueous reaction products resulting in change of mineralogy chemistry and texture

A

hydrothermal alteration

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72
Q

front or edge minerals was not completely replaced

A

vermicular intergrowths

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73
Q

concentric crustiform bands surrounding isolated fragments

A

cockade structures

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74
Q

formed when euhedral prismatis crystals of opposite walls merge with minerals takes place as single layer of euhedral crystals growing towards the center of the vein in epithermal systems

A

comb structure

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75
Q

colored bands that form when an electrolyte is allowed to diffuse into a gel being common in amorphous cryptocrystalline and microcrystalline minerals or mineraloids as agate and opal

A

liesegang rings

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76
Q

specific length and direction of systematic displacement by which the pattern is repeated

A

unit translation vector

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77
Q

the symmetry operation that involves the periodic repetition of nodes or motifs by systematic linear displacement

A

translation

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77
Q

symmetry operations that work as combined simple symmetry operations

A

compound symmetry operations

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78
Q

symmetry operation that combines translation parallel to an axis with rotation about the axis

A

screw rotation

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79
Q

groups denoted by their rotational and reflection symmetry

A

plane point groups

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80
Q

smallest units of meshes contains at least one node and the unit translation vectors

A

unit meshes

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81
Q

primitive and charac by unequal unit translation vectors that inersect at angles that are neither 60 degrees and 90 degrees nor 120 degrees

A

oblique

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82
Q

3d patterns of points produced from the translation of nodes of space point groups

A

space lattices

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83
Q

a parallelepiped whose edge lengths and volume are defined by the 3 unit translation vectors

A

unit cell

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84
Q

orientation of the unit cell edges

A

crystallographic axes

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85
Q

pair of faces symmetrical about an axis of rotation

A

sphenoid

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85
Q

the proportional lengths of the 3 crystallographic axes

A

axial ratio

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86
Q

or unit face any face or plane that intersects all 3 axes at distances from the center that correspond to the axial ration of the mineral

A

unit plane

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87
Q

method describing the relationships between sets of crystal faces or planes and the crystallographic axes

A

weiss parameters

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88
Q

reciprocal of weiss parameters

A

miller indices

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88
Q

represents what:

(h, k, l)
(hkl)
[hkl]
{hkl}

A

a point
a plane
a direction
family of planes

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89
Q

type of substitution that involves the simultaneous substitution of ions of different charges in two different structural sites

A

coupled ionic substitution

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89
Q

type of mineral growth where individual atoms and ions bons into a crystal’s nucleus and progressively grow by adding atoms/ions to its surface

A

homogeneous nuclueation

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90
Q

rock consists of multiple types of minerals and mineraloids

A

polyminerallic rock

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90
Q

type of mineral growth where a mineral nucleates by taking advantage of the structure of an existing mineral

A

hetegeneous nucleation

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90
Q

rock that consists of multiple crystals of a single mineral

A

monominerallic rock

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91
Q

liquid portion of magma composed mainly of mobile ions of the eight most abundant elements in the earths crust

A

melt

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91
Q

gaseous component of magma that will vaporize and turn into gas at surface pressures

A

volatile

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92
Q

partial melting of a source rock in the earths crust which produces a liquid melt fraction enriched in lower temperature constituents and a residual rock enriched in higher temperature refractory minerals

A

anatexis

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93
Q

results from crystallization along the walls of the magma chamber in which crystals prefentially form and adhere to the edges

A

marginal accretion

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93
Q

develops as the magma chamber walls release heat to the relatively cold country rock generating crystals that adhere to the side margins of the magma chamber

A

sidewall accretion

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93
Q

also called adabiatec melting is partial melting that resulted from a decrease in pressure

A

decompression melting

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94
Q

type of marginal accretion that results from early crystallization of minerals along the ceiling or the roof due to preferential heat loss

A

roof accretion

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95
Q

occurs as crystals forma long the base of the magma chamber

A

floor accretion

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96
Q

fractional crystallization process that occurs where liquids and crystals in a magma are separated due to factors like velocity density temperature

A

convective flow seggregation

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97
Q

process where a magma chamber squeezes out the more mobile liquid into a new chamber and leaving behind a residue of crystals in the original chamber

A

filter pressing

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98
Q

where one magma fractionates to produce two or more distinctly different daughter magmas with different compositions

A

liquid fractionation

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99
Q

involves the selective diffusion of ions in the magma due to compositional and may play a role in the generation of metallic ore deposits of ore deposits in magmatic systems

A

differential diffusion

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100
Q

separation of magma into two or more distinct immiscible liquid phases

A

liquid immiscibility

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101
Q

fracturing of the wall rock due to the forceful injection of the magma

A

stoping

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102
Q

country rock fragments

A

stope

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103
Q

stopes that fall into the magma

A

xenoliths

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104
Q

occurs along convergent margin environments with volcanic arcs and subduction zones decrease in iron and magnesium with increasing SiO2 alkali concentrations

A

calc-alkaline magmas

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105
Q
A
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106
Q

enrichment in iron at low to moderate SiO2 concentrations with increasing fractionation due to depleted MgO and Cao from early crystallization of forsterite olivine and Ca plagioclase. produce large volumes of basalt with little variations in composition. occurs extensional environments such as ocean ridges and ocntinental rifts and some hotspots in intraplate settings and immature arcs in thin volcanic arc crusts

A

tholeiitic magmas

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107
Q

magmas tha are less common than calc alkaline or tholeiitic magmas highly enriched in na2o and k2o contains diverse composition occurs in wide variety of environments that include stable cratons continental rifts and subduction zones

A

alkaline magmas

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108
Q

cahrac by high concentrations of silicic and basic rocks with little intermediate rocks and associated with continental rifts. basic component is derived from partial melting of the mantle while its silicic component is derived from the partial melting of the continental crust from the heating of the rising basic magmas

A

bimodal magma suites

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109
Q

45-55% SiO2
1,000-1200C
fluid
low gas

A

mafic (basaltic)

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110
Q

55-65%
800-1000 C
viscous
intermediate

A

intermediate andesitic

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111
Q

65-75%
650-800C
very viscous
high gas

A

felsic granitic

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112
Q

identify the magma type based on the percent of their silica content
<45%
45-52%
52-63%
63-68%
68-77%

A

ultramafic
mafic
intermediate
dacitic
felsic

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113
Q

plutons with an irregular shape that have surface exposures > 100 km2

A

stocks

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114
Q

veins that occur in great abundance that may display random or preferred orientations

A

vein swarms

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115
Q

carrot shaped and develops through explosive intrusions originating deep within the mantle

A

diatreme

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116
Q

multiple radiating dikes typically produced when the vertical forces of a rising magma fracture of the rock in a radiating pattern

A

radial dikes

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117
Q

dikes that are nearly vertical in cross section and circular in plan view

A

cone dikes

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118
Q

dikes that are circular in plan view but converge at a depth

A

cone sheet dikes

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119
Q

dike swarms consisting of parallel offset dikes that form in response to shear

A

en echelon dikes

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120
Q

steeply inclined set of dikes composed of gabbro diabase and basalt which form by cooling and contraction of magma as it is injected into extensional fractures in oceanic rift valleys

A

sheeted dikes

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121
Q

direct type of classification of composition that involves visual comparison of minerals and determining their volume percentages

A

modal classification

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122
Q

indirect type of classification of composition that analyzes the chemical composition of rocks

A

normative classification

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123
Q

dark or greenish rocks rich in olivine that may also contain pyroxene or amphibole

A

ultramafic or ultrabasic <45 %

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124
Q

dark colored rocks containing pyroxene amphibole olivine biotite

A

mafic basic 45-52%

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125
Q

grayish to salt and pepper colored rocks rich in plag amphibole biotite quartz

A

intermediate 52-66%

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126
Q

light colored or reddish rocks rich in k feldspar quartz biotite or muscovite

A

felsic acidic >66%

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127
Q
A
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128
Q

plutonic ultrabasic ultramafic rock enriched in pyroxene olivine amphibole and plag and occurs in earths mantle

A

peridotite

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129
Q

volcanic ultrabasic ultramafic rock enriched in pyroxene olivine amphibole and plag

A

komatiite

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130
Q

plutonic rock rich in plag pyroxene olivine in lower crust of ocean basins

A

gabbro

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131
Q

basalt volcanic rock rich in plag pyroxene olivine inupper earths crust

A
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132
Q

rich in hornblende pyroxene and plag

A

diorite( beneath andesite volcanoes) and andesite (pacific ring of fire)

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133
Q

plutonic light colored contains two thirds of SiO2 plag alkali felds quartz hornblende and biotite occurs beneath andesite dacite volcanoes

A

granodiorite

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134
Q

volcanic light colored contains two thirds of SiO2 plag alkali felds quartz hornblende and biotite occurs pacific ring of fire

A

dacite

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135
Q

acidic felsic rock rich in quartz and alkali felds contains little plag biotite

A

granite rhyolite

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136
Q

crystals too small for the naked eye but large enough to be identified with a petrographic microscope

A

microlites

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137
Q

fine grained material in porphyritic texture

A

groundmass

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138
Q

type of porphyritic texture where all crystals are visible to the naked eye but phenocrysts are distinctly larger than the groundmass

A

porphyritic-phaneritic

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139
Q

1-3 mm fine develop shallow plutonic dikes and sills
3-10mm develop in medium
10-33mm associated with larger or deeper intrusions

A

phaneritic

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140
Q

type of porphyritic texture where the phenocrysts are embedded in an aphanitic groundmass composed largely of microcrystalline cryptocrystalline or glassy material

A

porphyritic aphanitic

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141
Q

number of new seed crystals that develop per volume per unit time
nuclei/cm3/s

A

crystal nucleation rate

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142
Q

rate at wc elements migrate through magma that depends primarily on the viscosity of the melt

A

diffusion

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143
Q

elements that tend to increase molecular linkage wc increase viscosity

A

network formers

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144
Q

occurs when melts come into contact with air and water rapidly absorbing heat causing the melt to solidify rapidly before crystals could nucleate and grow

A

quenching

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145
Q

rounded masses of radiating crystals that debelop from devritification

A

spherulites

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146
Q

igneous rock texture charac by cloudy appearance and perlitic cracks

A

perlitic texture

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147
Q
A
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148
Q

curved or subspherical cooling cracks

A

perlitic cracks

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149
Q

glassy SiO2 rich volcanic rocks with perlitic texture and higher water contents than obsidian

A

perlite

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150
Q

depth where volatiles exsolve from the liquid as separate phase

A

level of exsolution

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151
Q

process that occurs above the level of exsolution where volatiles nucleate as small bubbles

A

vesiculation

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152
Q

encountered when bubbles constitute 70-80% of the magma volume and magma changes from a liquid with suspended gas bubbles to a buoyant gaseous mixture containing liquid blobs

A

fragmentation surface

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153
Q

rocks contain5-30% vesicles

A

vesicular

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154
Q

<5% vesicles

A

vesicle bearing

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155
Q

tuffs that contain significant amounts of gravel sized lapilli

A

lapilli tuff

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156
Q

pyroclastic rock primarily composed of blocks and deposited proximal to the volcano vent and subjected to minimal transport

A

volcanic breccia

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157
Q

composed of bombs that are abraded and rounded by transport

A

agglomerate

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158
Q

process in pyroclasts that results for fragments become progressively fused together as porosity decrease during compaction

A

welding

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159
Q

tuff that display random shard orientations and spherical to ellipsoidal pumice vesicles

A

unwelded tuff

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160
Q

tuff produced from increased volume of pyroclastic debris

A

partially welded tuff

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161
Q

tuff with dark colors and glassy lusters produced form intense welding with shards showing marked parallelism and flattening

A

densely welded tuff

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162
Q

first norm classification devised by Cross idding pirsson and washington

A

CIPW norm more

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163
Q

accurate metho of obtaining ga mode for any coarse grained rock done by moving a thin section on a gird system such that at least 400 minerals are tabulated for each thin section

A

point count analysis

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164
Q

0.0625-2mm
<0.0625

A

coarse ash
fine ash or dust

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165
Q

contains >69% SiO2 and assoicated with explosive silicic eruptions producing fragmental glassy and aphanitic

A

rhyolite

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166
Q

contains ~68-73% SiO2 not typically recognized by the IUGS as an official classification for rocks between rhyolites and dacites

A

rhyodacite

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167
Q

contains calciumplag and quartz with minor potassium feldspar biotite and hornblende

A

tonalite

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168
Q

plagiogranite are granodioritic rocks with half to two thirds sodium plag for the total felds

A

trondhjemite

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169
Q

produce low potassium arc theoiite basalts as well as relatively rare rocks such as boninites and adakites

A

young island arc systems

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170
Q

high mg intermediate volcanic rocks that contain a sio2 SATURATED GROUNDMASS

A

boninite

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171
Q

silica saturate rocks with high sr/y and la/yb ratios and low hfs concentrations

A

adakite

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172
Q

archean associations found in archean subduction zones where adakite formation is linked to

A

tonalite trondhjemite and granodiorite association TTG

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173
Q

arcs producing voluminous granodiorite diorite granite and tonalite plutons which can erupt onto the Earths surface and produce composite volcanoes

A

ocean continent convergent margins

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174
Q

dark colored potassium rich trachyandesites commonly containing olivine and augite phenocrysts with a groundmass of labradorite plag alkali fels livine augite and leucite

A

stoshonites

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175
Q

fault bounded deoformed rock sequences that mark the site of present of former convergent margins

A

alpine orogenic complexes

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176
Q

an internsely sheared heterogeous rock assemblage embedded within a highly deformed mud matrix

A

tectonic melange

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177
Q

greatest manifestations of intraplate magmatism on earth encompassing >10^6km3 in volume which occur as both oceanic flood basalts and continental flood basalts and is generally basaltic in composition

A

large igneous provinces LIP

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178
Q

geochemically distinct suite of rocks that are more alkalic less depleted and may be somewhat enriched with incompatible elements that is interpreted to represent different mantle sources areas

A

ocean island basalts OIB

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179
Q

huge outpourings of basalts within continental plates

A

continental flood basalts cfb

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180
Q

early jurassic
widley dispersed in the atlantic ocean places in north america south america europe and africa

A

cental atlantic magmatic province camp

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181
Q

251 ma
maymecha kotuy region of russia

A

siberian flood basalts (siberian traps)

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182
Q

65-69 Ma
southwestern india

A

deccan traps

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183
Q

15.5-17 ma
washington oregon and idaho usa

A

columbia river flood basalts

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184
Q

continental feature that produce a wide array of rocks including alkalic basalt as well as alkalic and silicic rocks

A

continental rifts

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185
Q

widespread occurrence of basalt and rhyolite without significant andesiteand occurs at continental rifts and hotpost underlying continental lithosphere

A

bimodal volcanism

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186
Q

anorogenic bodies injected into stable continental cratons at moderate depths

A

layered basic ultrabasic intrusions

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187
Q

ultrabasic volcanic rocks found exclusively in archean greenstone belts which are associated with valuable metallic ore deposits

A

komatiite

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188
Q

brecciated mg rich ultrabasic rocks that rapidly rise of earths surface via cylindrical diatremes from deep within the mantle and are intimately associated with diamonds

A

kimberlites

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189
Q

shallow intrusive to volcanic rocks that contain >20% CO3 minerals and form in stocks dikes and cylindrical structures primarily at continental rifts

A

carbonatites

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190
Q

mg rich volatile rich porphyritic rocks containing mafic phenocrysts and are associated with kimberlites and continental rift zones

A

lamprophyres

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191
Q

k rich peralkaline containing pyroxene and olivine minerals enriched in barium lanthanum and zirconium but poor in CO2 and occur in areas of thickened lithosphere that have experienced earlier plate convergence or rifting episodes

A

lamproites

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192
Q

contains economic deposits of platinum group metals chromium copper and nickel sulfides
exposed along a NW strike for a distance of 48 km iwith observable thickness of 6km
beartooth mountains of southwestern montana canafa
2.7 ga

A

stillwater complex

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193
Q

worlds largest layered igneous intrusion hosts the largest reserves of vanadium and chromium and platinum groups of metal in the world
PGE are concentrated within the merensky reeds critical zone
peridotite to gabbro from bottommost layer to topmost layer
400km in length up to 9 km thich and underlying an area 60 000 km2
south africa
2.06 ga

A

bushveld complex

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194
Q

youngest of the great PGE enriched intrusions
due to fractional crystallkization differentiation and convective currents its laye creates a complex layering
500 km3 volume
greenland
55ma

A

skaergaard intrusion

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195
Q

contact metamorphism
mon foliated
>80 C/km

A

contact

196
Q

40-80 C/ km
regional and contact metamorphism
foliated and non foliated

A

buchan (abukama)

197
Q

20-40C/km
regional metamorphism
foliated

A

barrovian

198
Q

10-20C/km
regional metamorphism
foliated

A

sangbagawa

199
Q

<10C/km
regional metamorphism at subduction zones
foliated

A

franciscan

200
Q

mass of proton in kg

A

1.67262192 × 10-27 kilograms

201
Q

how many rare elements in periodic table of elements?

A

17

202
Q

element that is very compatible and doesn’t substitute into major silicate phase

A

Zirconium

203
Q

Lanthanide series

A

The 17 rare earth elements are: lanthanum (La), cerium (Ce), praseodymium (Pr), neodymium (Nd), promethium (Pm), samarium (Sm), europium (Eu), gadolinium (Gd), terbium (Tb), dysprosium (Dy), holmium (Ho), erbium (Er), thulium (Tm), ytterbium (Yb), lutetium (Lu), scandium (Sc), and yttrium (Y).

204
Q

What is the rarest rare earth element?

A

Even the rarest rare earth, thulium, with atomic number 69, is 125 times more common than gold. And the least-rare rare earth, cerium, with atomic number 58, is 15,000 times more abundant than gold.

205
Q

focusing the eyepiece

A

diopter adjustment ring

206
Q

lies in the wavefront and is perpendicular to the ray vibration in isotropic media

A

vibration direction

207
Q

extinction angle of augite

A

inclined or 45 degrees

208
Q

permits measurement of refractive index by comparison of the unknown crystal with liquids of known refractive index. A determination of refractive index usually suffices for the identification of isotropic crystals.

A

The immersion method

209
Q

degree of visibility of a transparent mineral in an immersion medium

A

relief

210
Q

hardness of microcline

A

6

211
Q

where is ferropericlase abundant?

A

lower mantle

212
Q

crystal system of sphene

A

monoclinic

213
Q

clear variety of beryl

A

goshenite

214
Q

pink/orange variety of beryl
red variety of beryl
yellow variety of beryl

A

morganite
bixbite
heliodor

215
Q

known as vermillion

A

cinnabar

215
Q

lepidolite is a monoclinic mineral that belongs to a silicate group that has Si:O ration of

A

2:5

216
Q

variety of microcline that is very stable

A

amazonite

216
Q

crystal system of rhodonite

A

trinclinic

217
Q

known as moonstone

A

feldspar

218
Q

variety of hematite with metallic luster

A

specularite

219
Q

sanidine has a crystal system that has

A

no equal sides

220
Q

tennantite belongs to what group

A

sulfosalts

221
Q

cabochon gem is a

A

sulfide

222
Q

considered to be the heaviest nonmetallic ore

A

crested roses

223
Q

purple mica
magnesium mica

A

lepidolite
phlogopite

224
Q

found in lithium-bearing granite pegmatites.

A

spodumene

225
Q

prussic acid at crystalline is known as

A

zyklon A

226
Q

A mineral that has become virtually amorphous owing to the breakdown of the original crystal structure by internal bombardment with alpha particles (helium nuclei) emitted by radioactive atoms within the mineral.

A

metamict

227
Q

the replacement of one element in a crystal by another.

A

diadochic

228
Q

glossular is a Ca Al variety of granet and has a Si:O ratio of

A

1:4

229
Q

he most abundant mineral in the mantle.

A

Bridgmanite

230
Q

alumina saturation what do you call a rock that has a mineral assemblage of olivine clinopyroxene and orthopyroxene?

A

subaluminous

231
Q

where is low velocity layer found

A

60-220km

232
Q

rocks in immature oceanic island arcs containing olivine plag anda ugite with sparse othopyroxene and magnetite

A

low-k arc basalts

233
Q

represents the fertile unaltered mantle

A

lherzolite

234
Q

rocks contain phenocrysts of olivine chromite plag and augite with plag as the most abundant

A

mid oceanic ridge basalts

235
Q

black fibrous with a silky lustre friable and soft coal that represents fossil charcola

A

fusain

236
Q

also known as Steatite—is a metamorphic rock that consists primarily of talc.

A

Soapstone

237
Q

bright shiny black coal that usually breaks cubically and mostly consists of woody tissue

A

vitrain

238
Q

mineralogical adjustment of relatively high-grade metamorphic rocks to temperatures lower than those of their initial metamorphism.

A

Retrograde metamorphism

239
Q

develops in the outer fringes of many metamorphic aureoles

A

albite-epidote Hfls

240
Q

low pressure equivalent of the amphibole facies

A

hornblende hfls

241
Q

hypersthene bearing granitic gneisses

A

charnockite

242
Q

what does siliceous oozes forms

A

chert

243
Q

association of Bryozoa, Foraminiferida, coralline red algae (Rhodophyceae), and Mollusca that inhabits seas where the temperature often falls below 15°C

A

foramol

244
Q

an association of calcareous green algae (Chlorophyta), hermatypic corals, and molluscs (Mollusca) that lives in low latitudes, in seas where the temperature is always more than 20 °C

A

Chlorozoan

245
Q

an association of green algae (Chlorophyta), living in sea water more saline than corals could tolerate, that forms a characteristic calcareous sediment

A

chloralgal

246
Q

commonly intrude buoyantly upward along fractures or zones of structural weakness through denser overlying rocks.

A

Diapirs

247
Q

a method to keep solid particles floating in an upward direction (Figure 5) in a flow of gas or liquid.

A

Fluidization

248
Q

process in which sediments compact under pressure, expel connate fluids, and gradually become solid rock.

A

Lithification

249
Q

type of cement is formed at the sediment water and sediment air interfaces it is essentially syn sedimentary

A

eogenetic cement

250
Q

are banded coals. They are the most abundant type of coal. The bands of coal that comprise a humic coal are divided into four lithotypes (vitrain, clarain, durain, and fusain,

A

Humic coals

251
Q

hydrogen-rich coal, including cannel coal and boghead coal (see torbanite), derived from sapropels (loose deposits of sedimentary rock rich in hydrocarbons) and characterized by a dull black, sometimes waxy lustre.

A

sapropelic coal

252
Q

composed of mainly smectite clays that are alteration products of basaltic rocks

A

bentonite

253
Q

irregular solution surfaces consist of accumulation of iron oxides micas and insoluble minerals

A

stylotites

254
Q

e result of thin microscopic inclusions within a translucent mineral, usually as exsolution lamellae, which refract and reflect incident light.
play of colors reflections exhibited by labradorite and caused by internal structures that selectively reflect on certain colors

A

Schiller effects

255
Q

isinglass has a Si:O of

A

2:5

256
Q

material is either one which causes visible light to be split up into distinct beams of different wavelengths, or one in which light rays having different polarizations are absorbed by different amounts.

A

a dichroism

257
Q

a basalt that contains plagioclase feldspar (labradorite), clinopyroxene (augite with pigeonite), and iron ore (magnetite and ilmenite).

A

Tholeiitic

258
Q

a measure of the degree of oxidation in the rocks. It corresponds to the effective partial pressure of gaseous oxygen that would be in thermodynamic equilibrium with the material of interest

A

Oxygen fugacity

259
Q

involves prefential diffusion of select ions within the magma in response to compositional thermal or density gradients as well as water content

A

plastic flow

260
Q

what is a komatiite

A

ultramafic

261
Q

high aluminum basalt

A

arc–tholeiites

262
Q

what is lamproite

A

ultramafic

263
Q

formed by the contraction of clay in response to changes in the salinity of a liquid surrounding a deposit. shrinkage cracks form under water in clayey sediments

A

Syneresis cracks

264
Q

hornblende-biotite granite containing large round crystals of orthoclase each with a rim of oligoclase.

A

Rapakivi granite

265
Q

extremely acicular olivine phenocrysts–probably a sign of rapid crystallization from a significantly-undercooled magma. striking feature of ultramafic to mafic rocks that are interpreted to form in lavas or high-level intrusions when crystals cool in the presence of a thermal gradient

A

Spinifex textures

266
Q

what is golden paint

A

sulfide

267
Q

most eruptive volcanoes possess silicate mineral from which group

A

tectosilicate

268
Q

basaltic rock rich in olivine and augite phenocrysts on some the abundance of mafic phenocrysts may have been enhanced by gravitational accumulation

A

ankaremite

268
Q

a ring around an igneous intrusion. Deep magma bodies cool very slowly and turn into coarse-grained, plutonic rocks like granite and gabbro.

A

Aureole

269
Q

what mineral is not part of the greenschist facies

A

omphacite (clinopyroxene)

270
Q
  • large, heavy pebbles are rolled along the river bed. This is most common near the source of a river, as here the load is larger.
A

Traction

271
Q

laumonite and heulandite are index minerals of

A

zeolite facies

272
Q

depth of subducting slab required for a volcano to manifest at the surface

A

100km

273
Q

fragmented comagmatic volcanic rocks from prev eruptions of the same volcano

A

cognate clast

274
Q

A diagram that shows the amount of each of the chemical constituents of a rock as a proportion of the main ingredient

A

Harker diagram

275
Q

illite is a

A

3 layered clay

276
Q

composition is omphacite and pyrope which is a red garnet and with small amounts of diopside enstatite olivine kyanite rutile and diamond

A

eclogite

277
Q

characterized by a porphyritic texture in which abundant large crystals of dark colored minerals are set in a note visibly crystalline matrix

A

lamprophyre

278
Q

shaped like a football or spindle of thread; others, called cow-dung or pancake bombs, are flattened on landing; and still others are ribbon-shaped.

A

spindle bomb

279
Q

created when the upward pressure of slow-moving molten lava within a flow swells or pushes the overlying crust upward. fomrs ovoid mounds few feet high and a few tens of feet long produced from the buckling up of hardened outer edges and surfaces

A

tumuli lava

280
Q

a rare mineral Na6Mg2(SO4)(CO3)4 that is an octahedral sulfate and carbonate of sodium and magnesium (

A

tychite

281
Q

the property of changing from one mineral species to another (as from aragonite to calcite) by a change in internal structure and physical characters but not in chemical composition

A

Paramorphism

282
Q

clast supported with >2mm sized components

A

rudstone

283
Q

act as a heat sink and provides the mass for mobile phone vibration

A

wolframite

284
Q

ingredient in toothpaste for sensitive teeth

A

strontium

284
Q

mineral used in storage of radioactive waste

A

pollucite

285
Q

chromophore in blue dimaonds

A

boron

286
Q

chromophore in morganite

A

manganese or caesium.

287
Q

used in incandescent light bulb as protective layer around filament to keep oxygen from corroding it

A

Argon

288
Q

key ingredient in processing aluminum and uranium

A

fluorite

289
Q

used in ree magnets lasers ceramic capacitors and electric motors of electric automobiles

A

neodymium

290
Q

used in making microwave filters for radar

A

yttrium

291
Q

what is the streak of galena

A

lead gray

292
Q

mindoro jade is composed of

A

sericite schist

293
Q

cleavage angle of hornblende

A

56 124

294
Q

mg rich chlorite

A

clinochore

295
Q

the fe bearing analog of talc

A

minnesotaite

296
Q

serpentine group

A

(antigorite, lizardite, and chrysotile).

297
Q

eutectic point of aluminum silicate diagram

A

500-550 degrees celcius

298
Q

streak of hematite

A

bloody red

299
Q

streak of chromite

A

brown

300
Q

gold telluride, is an uncommon telluride of gold, a metallic mineral with the chemical formula AuTe2, with approximately 3% of the gold

A

Calaverite

301
Q

ores of gold

A

old-polysulfide, gold-quartz, gold-telluride, gold-tetradymite, gold-antimony, gold-bismuth-sulfosalt, gold-pyrrhotite, and gold-fahlore.

302
Q

difference perthite and antiperthite

A

If K-feldspar predominates, it is a perthite. If Albite predominates, it is an antiperthite.

303
Q

high-magnesium olivine basalt that is very rich in the mineral olivine. It is dark with yellow-green olivine phenocrysts and black to dark brown pyroxene, mostly augite.

A

picrite phenocrysts sa augite olivine

304
Q

a chemical reaction in which the type of chemical bonds broken in the reactant are the same as the type of bonds formed in the reaction product.

A

An isodesmic reaction

305
Q

outside of the pyroclastic bomb solidify during their flight

A

Breadcrust bomb, dacite
volcanic bomb with a cracked and checkered surface, sometimes resembling the surface of a loaf of bread.

306
Q

alteration product of devitrification or volcanic glass alteration

A

palagonite

307
Q

to mark with two series of parallel lines that intersect.

A

crosshatched

308
Q

special type of extinction by micas such as biotite and muscovite and also carbonates such as calcite and dolomite

A

mottled extinction

309
Q

important application related feature of the objective. It is the distance between objective front end and coverslip surface facing the front lens

A

free working distance

310
Q

refractive index of canada balsam

A

1.53

311
Q

used to remediate spills or remove waste products from liquids

A

absorbents

312
Q

inert inexpensive materials that extend the volume of material at low cost

A

fillers

313
Q

fourth most abundant element in earth

A

Magnesium
take note of the word earth!

314
Q

intraformational rudites tend to form this

A

breccia

315
Q

4 fold axis rotation that coincides with c crystal axis

A

tertagonal

316
Q

minerals or synthetic inorganic crystal phases that have high melting points. They should also be resistant to deformation and to softening at high temperatures.

A

Refractory minerals

317
Q

meteorites that document melting and segregation in planetesimals and are consist of olivine crystals in an iron nickel matrix

A

pallasite

318
Q

not an indicator of high pressure and low temperature

A

laumonite

319
Q

develops in response to geothermal gradients of ~20 - 40 degrees c/km reflecting the progressive increase in both temperature and pressure during regional metamorphism

A

barrovian FS

320
Q

records high geothermal gradients ranging from 40 to 80 degrees c/km

A

abukuma FS

321
Q

facies that form at convergent plate margins in ophiolite complexes and subduction zone melanges

A

blueschist

322
Q

non plastic clay that can be used to decolorise, filter and purify animal, mineral and vegetable oils and greases.

A

Fuller’s earth

323
Q

commonest member of the kandite group and is generally formed in soil profiles in warm humid envi where acidic waters intensely leach bedrock lithoogies such as granite

A

china clay

324
Q

forms under medium temperature 350-550 C and pressure 3-10 kbar 10-30 km depth conditions associated with dynamothermal metamorphism at convergent plate boundaries

A

greenschist facies

325
Q

Dark in color, containing at least 50-60% mafic minerals.

A

mesocratic

326
Q

Said of igneous rocks that consist of 90% to 100% mafic minerals.

A

hypermelanic

327
Q

developed during hydrothermal alteration at divergent margins hotspots and convergent margins or during burial metamorphism at depths less than 5km

A

zeolite facies

328
Q

metamorphic facies formed in convergent plate margins like orogenic fold and thrust belts which are charac by moderate temperature/ pressure metamorphic conditions

A

greenschist

329
Q

also termed soluviation, ferrallitization, laterization,and latosolization) produces aluminium hydroxidessuch as gibbsite.

A

allitization

330
Q

The development of amphibole from pyroxene; specif. a late-magmatic or metamorphic process of replacement whereby uralitic amphibole results from alteration of primary pyroxene

A

uralitization

331
Q

the replacement of original skeletal material accomplished through the concurrent dissolution of calcium carbonate and precipitation of silica

A

Silicification

332
Q

a model of global mean sea level that is used to measure precise surface elevations

A

geoid

333
Q

minimum size of objects that can be detected by a sensor system

A

spatial resolution

334
Q

cyanide spill in rapurapu

A

lafayette ph inc.

335
Q

a homogeneous national network of geodetic control points marked by concrete monuments or mojons that has been established using Global Positioning System technology

A

PRS92

336
Q

easting value refers to

A

longitude

337
Q

company that was involved in the disaster that killed Boac River

A

Marcopper Mining corp

338
Q

sufficient information clear and unambiguous presentation of data not misleading to the readers of the public report

A

transparency

339
Q

age of pacific plate

A

Late Jurassic

340
Q

how many organic matters produced were preserved in petroleum reesource

A

0.1%

341
Q

the basement of masbate island

A

metamorphic complex

342
Q

ore bearing fluid rich in Na and Cl contain Ca Mg HCO3 and many contains Sr-Ba-N

A

connate water

343
Q

also called metallogenic zoning

A

regional zoning

344
Q

net movement of anything generally from a region of higher concentration to a region of lower concentration. Diffusion is driven by a gradient in Gibbs free energy or chemical potential.

A

Diffusion

345
Q

is the coexistence of two or more liquid phases in equilibrium. Petrogenetic interest has stemmed from the potential of a homogeneous magmatic liquid to separate a second liquid phase in response to a change in temperature, pressure or composition.

A

Liquid immiscibility

346
Q

type of magmatic fluid enriched by Sn-W-Be-Li

A

S type granite

347
Q

alloy of Pb and Sn

A

Solder

348
Q

alloy of gold and copper

A

tumbaga

349
Q

areas with coal reserve

A

south mindoro
SIBUGUEY PENINSULA
samar

350
Q

a right lateral fault

A

aglubang fault

351
Q

basement of northern northern sierra madre

A

angat ophiolite

352
Q

dirty or loose connections between the geophones and the cable or the cable and the recording system

A

electronic noise

353
Q

later time of arrival of the reflected rays at receivers offset from the source for a horizontal reflector

A

normal waveout

354
Q

age of semi anthracite deposit of catanduanes

A

eocene

355
Q

cylindrical metal tube whichhouses the instrumentation needed for borehole logging

A

probe

356
Q

age of celebes sea basin

A

eocene

357
Q

basement of bondoc

A

gumaca schist

358
Q

age of manila trench

A

15Ma

359
Q

basin with the same classification

A

bicol shelf
illocos trough
agusan davao basin

360
Q

by product of coal processing

A

sulfur

361
Q

converting electrical energy into acoustic energy
this has the highest frequency

A

sparkers
boomers

362
Q

west linapacan

A

oil field

363
Q

sara diorite is found where

A

panay

364
Q

calatrava qartz diorite is found where

A

tablas

365
Q

act practive of geology in the ph

A

10166

366
Q

act geology profession act of pg

A

ra 4209

367
Q

ph mining act

A

ra 7942

368
Q

ra 8371

A

indigeneous rights

369
Q

when was the geological society of the philippines was established

A

1945

370
Q

line orientations in space relative to geographic directions

A

compass bearing

371
Q

the small metal used in the compass to balance the needle

A

wire coil

372
Q

unit used for coal capacity to generate electricity

A

Btu/lbs

373
Q

far south east deposit is what type of deposit

A

porphyry base metal deposit

374
Q

eagle cement in bulacan

A

open pit mining

375
Q

age of dupax diorite

A

oligocene

376
Q

coal bearing formation in quezon province

A

bordoes fm

377
Q

barite is seen where

A

batangas

378
Q

clean water act

A

ra 9275

379
Q

kapoas granite

A

north palawan

380
Q

unit used for coal capacity to generate energy

A

Btu/lbs

381
Q

basin form in the same group

A

SE Luzon Basin
Cagayan Basin
Sulu Sea Basin

382
Q

which particle sized hosted large amount of organic matter

A

clay with less than 2 microns

383
Q

The last stage of maturation and conversion of organic matter to hydrocarbons. occurs at temperatures of 150 to 200 degC

A

Metagenesis

384
Q

eroded or reworked organic matter

A

Type IV

385
Q

former head of department of geology and geography of the university if the philippines was unanimously elected as first presdient of the geological society of the ph september 2, 1945

A

Dr. Jose Feliciano

386
Q

8.0 magnitude Moro Gulf happened when

A

1976

387
Q

when was the lexicon of ph stratigraphy published and who was the author and he was the presidnet of GSP on what year

A

2008 mr. rolando pena
1997

388
Q

sorsogon has what type of coal

A

sub bituminous coal

389
Q

age of zambales ophiolite

A

eocene

390
Q

feb 2012 negros earthquake had a magnitude of what

A

6.9 Ms

391
Q

what pd is the DOE

A

PD 1206

392
Q

BOOK INFORMATION ON THE VALEY FAULT SYSTEM PUBLISHED BY phivolcs

A

the valley fault system ATLAS

393
Q

PNOC established through

A

Presidential Decree No. 334

394
Q

title of the journal first released by GSP

A

the philippine geologist

395
Q

father of ph geothermal

A

arturo pineda alcaraz

396
Q

tsunami has not yet been verified could exist andmay be little as an hour away

A

tsunami watch

397
Q

used for petroleum extraction to mechanically lift fluid out of the well if not enough bottom hole pressure exists for the liquid to flow all the wat to the surface

A

PUMP JACK

398
Q

an anomaly that can be developed to be prospect with additional data

A

lead

399
Q

major type of seal in a petroleum system

A

mudstone

400
Q

how many percent of gas reserve is stored in limestones

A

30%

401
Q

indo aus plate is moving at

A

10.7 cm/yr

402
Q

where is the ph island moving direction

A

NW direction
due to the ph sea plate moving direction

403
Q

age of shikoku basin

A

10Ma

404
Q

ancient volcanic arc active between 20-9 Ma

A

west marianas ridge

405
Q

collision of the ph sea plate and eurasian plate at

A

4Ma

406
Q

sulu sea basin formed during

A

early miocene

407
Q

using vitrinite reflectance what is the color of the mature source

A

bluish tint

408
Q

survey used for cloudy terrane

A

RADAR

409
Q

calamian island according to PTM belongs to

A

Zone II

410
Q

difficult to perform overlaying
depends on the source data
occupies less space

A

vector

411
Q

resolution depends on the cell size
difficult to perform network analysis
suffers from discretization

A

raster

412
Q

the horizontal angle between the direction of an object and another object, or between it and that of true north.
machine element that constrains relative motion to only the desired motion and reduces friction between moving parts

A

bearing

413
Q

makes an assumption that the gravity station is flat and on land this is subtracted

A

bouguer correction

414
Q

velocity varies with depth so time cannot be easily converted to depth
may be multiple reflections off of a single interfaces
vertical scale on seismic reflection profiles is time not depth

A

seismic reflection survey

not (reflections occur parallel to the interface)

415
Q

data produced by SRTM

A

DEM

416
Q

comprise of rigid aluminium plate attached below a heavy duty electrical coil by a spring loaded mounting

A

boomers

417
Q

responsible for the awarding of private gratuitous permit

A

provincial governor

418
Q

provides activities to achieve mine closure

A

FMRDP

419
Q

no go zone

A

EO 79

420
Q

Renewable Energy Act of 2008’ was codified in December 2008 to affirm the government’s commitment to accelerate the utilization of renewable energy (RE) resources in the country.

A

Republic Act No. 9513

421
Q

what ra is this the geologist should practice

A

candor
intergrity
fidelity

422
Q

deposits form at or near the sea floor where the circulating hydrothermal fluids driven by magmatic heat are quenched through mixing with bottom waters or pore waters in near seafloor lithologies

A

volcanogenic massive sulfide

423
Q

formed continuous cooling differentiation and crystallization of intermediate silisic magmas

A

hydrothermal fluid

424
Q

also known as replacement deposti

A

skarn

425
Q

minerals that are typical of hosting ore deposit

A

chalcophile

426
Q

siruma mineral reservation is for what type of deposti

A

china clay

427
Q

pryhotite is an indicator mineral in what type of deposits

A

low sulfidation epithermal deposit

428
Q

vuggy quartz indicates

A

high sulfidation

429
Q

elevated value of Dy and Nd indicates

A

continental crust

430
Q

major ore for REE

A

bastnasite

431
Q

refer the prograding process

A

potassic and prophylitic

432
Q

defines D vein

A

pyrite vein + quartz with alteration halo

433
Q

type of VMS that is ophiolite related

A

cyprus tpye

434
Q

minerals contain REE and doesnt

A

xenotime
haloysite
chamosite

doesnt monazite

435
Q

amount of sample sufficient for geochemical analysis

A

0.20kg

436
Q

mineral extraction like heacy minerals minimum mass required for mass sampling

A

1000g-2000g

437
Q

asked a sample for XRD

A

collect a chipped sample

438
Q

depth soil profile appropriate for a sample

A

at least 1m

439
Q

sampling for bed for relative dating

sampling graded beds

A

lower portion of the bed

mark first the upward position

440
Q

soft
resistant to chemical corrosion
flexible

A

asbestos

441
Q

locality asbestos is found

A

antique
pangasinan
bukidnon

442
Q

barite is used as

A

extender

443
Q

deposit of fire clay found in

A

semirara

444
Q

feldspar deposit found in

A

occidental mindoro

445
Q

where is gypsum found

A

cebu
occidental mindoro
batangas

446
Q

perlite used as

A

insulator

447
Q

talc is found here

A

mindoro occidental
palawan
zambales

448
Q

quarry are granted by

A

provincial governor

449
Q

ideal state of geochemical analysis

A

powedered form

450
Q

magnesium is better mined in

A

seawater

451
Q

minerals that are supergene

A

anglesite
smithsonite
hemimorphite

452
Q

deepwater horizon oil spill happened in

A

gulf of mexico

453
Q

who is the chief operationg officer in a mining company

A

mining superintendent

454
Q

used to prevent salt flocculate of bentonite and minimize the effect of high temp gelatin in bentonite fluid and sometimes added to get better filtration control

A

ferrochrome lignosulfonates

455
Q

nickel deposit in sudbury

A

magmatic deposit

456
Q

barite in a gold vein deposit is

A

gangue

457
Q

max weigh of gold bar or disc accepted by BSP

A

5000g

458
Q

what is accepted and not accepted in BSP

A

accepted
not damp
in a fom of bar
in a form of disc

not
amalhamated

459
Q

count of existing FTAA in oh

A

5

460
Q

grants the application permit

A

director

461
Q

type of epigenetic ore

A

epithermal gold deposit
skarn deposit
porphyry deposit

not bauxite deposit

462
Q

levigation is appropriate to use

A

platinum
chromite
hematite

not in feldspar

463
Q

process of extracting one material from another by washing with a solvent as in washing of loaded ion exchange resisn to remove captured ions used by FCF in extracting gold by electrowinning

A

elution

464
Q

ASTER means

A

activated sludge tailing effluent remediation

465
Q

EIS is under

A

PD 1856

466
Q

ipra IS ALSO known as

A

8731

467
Q

has white alteration

A

lead

468
Q

used in medicine such as loparamide

A

palygorskite

469
Q

> 200 degrees C and one of the most useful geothermometer in finding geothermal resources

A

EPIDOTE

470
Q

indicates good permeability and process of boiling

A

adularia

471
Q

also known as coking coal

A

metallurgical coal

472
Q

past atmospheric composition indication

A

bubbles present in glaciers

473
Q

type of mining method used to mine coal

A

long wall

474
Q

used to extract mineral deposits that are roughly tabular and generally associated with strong ore and surrounding rock

A

unsupported method mining

475
Q

alizarine red S

calcite and aragonite will stain to
witherite
cerussite

A

pink orange
red
mauve

476
Q

trypan blue
calcite
dolomite

A

dark blue
pale blue

477
Q

silver chromate stain
calcite
aragonite

A

red brown

478
Q

copper nitrate stain
calcite

A

green/bluish green

479
Q

cobalt nitrate stain
aragonite

A

lilac-purple

480
Q

harris hematoxilin solution stain
calcite

A

lilac

481
Q

meigen stain to
aragonite
calcite

A

purple
no change

482
Q

rhodizonic acid stain
witherite
calcite

A

orange/red
no change

483
Q

tropaeolin
smithsonite
magnesite

A

yellow
no change

484
Q

hydrogen peroxide potassium hydroxide
ankerite
siderite

A

orange
brown

485
Q

lemberg hydroxide stain
calcite

A

plae brown

486
Q

bensideme
rhodochrosite

A

blue

487
Q

potassium ferricyanide
anhydrite/gypsum
rhodochrosite
dolomite

A

yellow
pale brown
blue

488
Q

organic dye titan yellow
dolomite

A

dark orange red

489
Q

organic dye eosin y
dolomite

A

dark pink

490
Q

organic dye congo red
dolomite

A

red

491
Q

oragnic dye alizarine red
dolomite

A

lilac

492
Q

feigl solution
aragonite

A

black

493
Q

sodium cobaltinitrite
k felds
plafs except albite

A

yellow
red

494
Q

kirchberg
ankerite
siderite

A

gray to black
little coloring

495
Q

magneson
smithsonite removed after washing
magnesite stays after washing

A

slightly blue
dark blue

496
Q
A