diagnostic Flashcards

1
Q

this forms the coastal folded belt of northern luzon and extends north and south between the high cordillera central and south china sea

A

ilocos basin

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2
Q

temperature wherein diagenesis occur

A

200C

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3
Q

product of extremely high grade regional metamorphism resulting into partial melting

A

migmatite

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4
Q

difference of speleothems and speleogens

A

Speleothems are formed over thousands of years and are deposited on top of the existing cave. Speleogens are similar but form inside the bedrock at the same time as the cave.

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5
Q

uses a 3d spherical surface to define locations on Earth

A

Geographic Coordinate System

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6
Q

divides the world into sixty north-south zones, each 6 degrees of longitude wide. UTM zones are numbered consecutively beginning with Zone 1, which includes the westernmost point of Alaska, and progress eastward to Zone 19, which includes Maine.

A

The UTM (Universal Transverse Mercator) coordinate system

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7
Q

the result of very high shear stress, such as occurs along fault zones. Dynamic metamorphism occurs at relatively low temperatures compared to other types of metamorphism, and consists predominantly of the physical changes that happen to a rock experiencing shear stress.

A

Dynamic metamorphism

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8
Q

occurs when low-grade or unmetamorphosed rocks change mineralogy or texture in response to a temperature increase.

A

Prograde metamorphism

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9
Q

what is the oh stratigraphic groupings

A

southwest luzon uplands

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10
Q

proposed extrusion tectonic to explain the formation of the South China Sea

A

Taponnier

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11
Q

typhoon to have a landfall over the Mindanao Island in December 2012 and the name was retired due to its high casualty and damages

A

Typhoon Pablo

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12
Q

will form in a metamorphic envi and when carbon is subjected to heat and pressure

A

graphite

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13
Q

linear trough of subsidence of the Earth’s crust within which vast amounts of sediment accumulate.

A

geosyncline

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14
Q

there were 4 main mobile belts that formed in the paleozoic namely franklin cordilleran applachian and

A

ouachita

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15
Q

discovered in a cave in the St. Paul Limestone Formation in Palawan PH

A

Sirenia (dugongs and manatees)

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16
Q

what are these

manidae
primates
dermoptera

A

pangolins
primates
flying lemurs

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17
Q

direct implication of the opening of the China Sea

A

movement of the palawan microcontinental block from mainland china

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18
Q

what is the taiwan collision zone charac as

A

continent-arc

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19
Q

in soil temperature regimes the PH islands most likely belong to what category

A

isohyperthermic

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20
Q

what does proglacial means

A

in front of the glacier

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21
Q

rare extrusive and intrusive igneous rocks that are silicic and sodium-rich. They were originally associated with the subduction of young oceanic lithosphere (≤ 25 Ma); however, they are now also commonly identified in non-subduction zone settings.

A

Adakites

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22
Q

any orthopyroxene-bearing quartz-feldspar rock formed at high temperature and pressure, commonly found in granulite facies’ metamorphic regions, sensu stricto as an endmember of the charnockite series.

A

Charnockite

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23
Q

type of plutonic igneous rock containing quartz (20 – 60% of the felsic minerals) and abundant plagioclase.

A

Tonalite

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24
Q

this crystallizes in the isometric system

A

pyrite

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25
Q

is a sequence of sedimentary rock layers that progress from deep-water and turbidity flow deposits to shallow-water shales and sandstones. It is deposited when a deep basin forms rapidly on the continental side of a mountain building episode.

A

Flysch

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26
Q

thick association of continental and marine clastic sedimentary rocks that consists mainly of sandstones and shales formed as shore deposits and refers to sandstones, shales and conglomerates that form as terrestrial or shallow marine deposits in front of rising mountain chains.

A

Molasses

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27
Q

what kind of rock is zambales jade?

A

uvarovite
chromium-bearing garnet group species

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28
Q

major type of seal in petroleum system

A

mudstone

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29
Q

where does stilbite belong?

A

zeolite

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30
Q

also known as siliceous sinter

A

geyserite

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31
Q

<10
5 calsilicate minerals, 0-20% mica 80-100 quartz + feldspar

A

psammite

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32
Q

high growth and high nucleation rates lead to what kind of texture

A

aphanitic

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33
Q

texture usually restricted to coarser grained rocks that consists of concentrically banded spheres wherein the bands consist of alternating light colored and dark colored minerals

A

orbicular

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34
Q

rare group of ultrapotassic igneous rocks charac by the presence of phenocrysts of mica and amphibole

A

lamproites

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35
Q

a term that may be used for a light colored <10% alkali feldspar granite

A

alaskite

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36
Q

a low-relief, broad volcanic crater formed by shallow explosive eruptions. The explosions are usually caused by the heating and boiling of groundwater when magma invades the groundwater table.
lower than scoria cone and has much larger central crater relative to the deposited ring of debris

A

maar

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37
Q

tactite is a synonym of which metamorphic rock

A

skarn

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38
Q

leuco-tonalite also known as

A

trondhjemite

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39
Q

what does CIPW stands for?

A

Cross, Iddings, Pirsson, and Washington.

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40
Q

chlorite + actinolite +/- albite +/- epidote

A

greenschist

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41
Q

high-grade metamorphic rocks of the granulite facies that have experienced high-temperature and moderate-pressure metamorphism.

orthopyroxene+clinopyroxene+plag+garnet

A

granulite

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42
Q

characterized by the minerals jadeite, glaucophane, epidote, lawsonite, and garnet.

A

blueschist

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43
Q

high-pressure, moderate-temperature conditions and typically characterized by the development of the mineral assemblage pyrope garnet and omphacite

A

Eclogite facies

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44
Q

facies charac by high pressure and moderate temp

A

sanbagawa

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45
Q

high temperature-low-pressure metamorphism and implies a higher geothermal gradient than in other regional metamorphic settings

A

Buchan-type

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46
Q

series of rocks that pass through the Zeolite, Prehnite-Pumpellyite, Blueschist, and Eclogite Facies of Regional Metamorphism

A

Franciscan Facies Series

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47
Q

flood basalt province had a peak volcanic activity around 65 MA which is close to the cretaceous tertiary extinction event

A

deccan

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48
Q

law states that angles between equivalent faces of crystals of the same mineral are always the same

A

steno’s law

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49
Q

the crystal class or point group 23 belong to which crystal system

A

isometric

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50
Q

softest mineral in talmage hardness scale denoted by A

A

acanthite

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51
Q

leucite, nepheline, sodalite, and lazurite vishnevite

A

feldspathoid

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52
Q

chemical formula of pyroxene

A

XYSi2O6

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53
Q

diposide hedenrbergite and augite are classified as

A

calcic clinopyroxene

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54
Q

synonym for vesuvianite

A

idocrase

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55
Q

The high density of these minerals gives rise to a qualitative property called Experienced geologists can roughly assess specific gravity
minerals density obtained by picking up the mineral and holding in your hand

A

“heft.”

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56
Q

deep red colors of gemstones is caused by small amounts of which element

A

chromium

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57
Q

composition of chert

A

quartz

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58
Q

crystal in which the strenght of all bonds from a cation to its coordinating anions is equal to exactly one half the charge of the anions

A

mesodesmic

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59
Q

locally known as adobe

A

tuff

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60
Q

the only known deposit of zeolite in ph is found in

A

mangatarem pangasinan

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61
Q

. The reference plane, or _____, from which elevations are measured for topographic maps, is
the mean (average) sea level.

A

Datum

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62
Q

. Assuming a zinc deposit is altering a dolomite rock, the isotope of which element can be used
to trace the orebody?

A

Strontium

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63
Q

The Geological Society of the Philippines (GSP), the only accredited integrated professional
organization of geologists in the Philippines by PRC, was established on

A

September 2, 1945

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64
Q

The volcano that erupted in 1951 which led to approximately 500 casualties

A

Hibok-hibok

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65
Q

The equation which yields the rate at which groundwater can pass through a unit area of
aquifer perpendicular to the flow

A

Hydraulic conductivity

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66
Q

. A type of ore-bearing fluid usually involved in the formation of evaporites and phosphorites

A

Seawater

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67
Q

The best-studied meteorite in history”

A

Allende

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68
Q

A type of kerogen in which its origin is from Phytoplanktons, bacterial microorganisms in
marine sediments. It is also the most abundant.

A

Type II Kerogen

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69
Q

Why is ventilation required in underground coal mining?

A

Due to elevated Methane released as Coal is being mined

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70
Q

In the origin and maturity of kerogen and petroleum, which carbonaceous material or
hydrocarbon is typically formed last?

A

Graphite

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71
Q

Which of the following has the least favorable environment for a High Sulfidation and Low
Sulfidation deposit to occur:

A

Granitic intrusions

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72
Q

The magnitude 7.8 earthquake that occurred last February 6, 2023, took place within the
vicinity of a triple junction between which plates?

A

Anatolia, Arabia, and Africa plates

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73
Q

What is the DENR Administrative Order that lifted the ban on open-pit mining of copper, silver,
gold, and complex ores in the country, and who initially enforced the said ban?

A

DAO 2021-40, Gina Lopez

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74
Q

what are the percents of these for the slope angle ranfes acc to the DENR slope classification

0-3%
3-5%-8%
8%-18%
18%-30%
30%-50%
over 50%

A

level to nearly level
gently sloping to undulating
undulating to rolling
rolling to moderately steep
steep
very steep

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75
Q

The parent magma believed to have released the fluid that accumulated to form the copperand gold-bearing quartz body in the Didipio orebody is of what comp

A

Syenitic

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76
Q

The Board of Geology was created in accordance with the Geology Profession Law to
supervise and regulate the practice of the geology profession. The Board of Geology was first
created in the Philippines in

A

June 19, 1965

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77
Q

Most coordinate systems used in GIS software correspond to a specific code set by the
European Petroleum Survey Group for the purpose of maintaining a geodetic parameter
database. What is the EPSG code for the widely used coordinate system World Geodetic System
84 (WGS 84)?

A

EPSG:4326

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78
Q

these codes represent which

EPSG:4269
EPSG:4326
EPSG:4253
EPSG:4683

A

NAD83
WGS84
Luzon 1911
PRS92

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79
Q

What is the difference between nautical mile and statute mile?

A

NM is longer than SM
NM 6076 feet SM=5280 feet

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80
Q

what are the respective percents for the Copper percentage
bornite
chalcopyrite
covellite
chalcocite

A

63.3%
34.63%
66.46%
79.85%

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81
Q

. Bronze is an alloy of what elements?

A

Cu and Sn

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82
Q

Dubbed the “worst oil spill ever in the Philippines”, the oil tanker M/T Solar 1 sank on August
11, 2006, releasing as much as 500,000 liters of crude oil in the vicinity of the wreck. Where did
the M/T Solar 1 sink?

A

Guimaras Strait

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83
Q

An oil with an API Gravity of 22.3–31.1 is considered as

A

Medium oil

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84
Q

According to R.A. 7076, upon the declaration of a people’s small-scale mining area, the
director, in consultation with the operator, claim owner, landowner, or lessor of an affected area,
shall determine the right of the small-scale miners to existing facilities such as mining and logging
roads, private roads, port, and communication facilities. This is known as

A

Easement rights

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85
Q

what are the RQD if thes rock quality

0-25%
25-50%
50-75%
75-90%
90-100%

A

very poor
poor
fair
good
excellent

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86
Q

What deposit garnered attention and controversy due to the misrepresentation of its resource
which led to the creation of JORC?

A

Poseidon Nickel Deposit – Poseidon NL

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87
Q

. A ‘Competent Person’ must have a minimum of _____ relevant experience in the deposit style
investigated

A

5 years

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88
Q

the most effective seal rock?

A

Evaporites

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89
Q

Which formation can one find the skarns in Larap?

A

Universal Formation

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90
Q

What mine is controversial because of a massive tailings spill incident in 1996?

A

Marcopper Cu Mine

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91
Q

Diwalwal gold rush started in what decade?

A

1980s

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92
Q

what article of the GSP Code of Ethics stipulates the relation of geologists to coprofessionals?

A

IV

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93
Q

This sets out the minimum standards, recommendations, and guidelines for public reporting
in the Philippines of exploration results, mineral resources, and ore reserves.

A

PMRC

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94
Q

Which of the following uses a logarithmic scale?

A

Richter Scale

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95
Q

. These isolines in maps indicate equal gravitational acceleration

A

isogal

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96
Q

Size Hole (outside) diameter, mm Core (inside) diameter, mm
AQ
BQ

NQ

HQ

A

48 27
60 36.5
75.7 47.6
96 63.5

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97
Q

What is added to quicklime to make morta

A

Clay

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98
Q

This is used to measure the rate of change in a magnetic field.

A

Gradiometer

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99
Q

What is the test similar to the Becke Line Test but used in mineragraphy?

A

Kalb Light Line

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100
Q

The characteristic ore mineral assemblage and their sequence of formation

A

Paragenesis

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101
Q

In variograms, this represents the maximum distance at which sample pairs can be said to
have some relationship to their separation distance

A

range

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102
Q

What is the true dip of the coal seam?

A

11SE

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103
Q

At what depth would the coal be encountered in a borehole at D?

A

200m

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104
Q

Where is the type locality of the mineral Luzonite?

A

Mankayan, Benguet

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105
Q

Which of the following countries has the most REE reserves?

A

China

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106
Q

Developed just in recent years, IFSAR is a powerful approach in generating high-resolution
digital data using Digital Elevation Model (DEM) and an orthorectified radar image. IFSAR stands
for what?

A

Interferometric Synthetic Aperture Radar

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107
Q

correlation analysis
+- 1
+-0.81-0.99
+-0.61-+0.80
+-41-0.69
+_0.21-+-0.40
+-0.01-+-0.20
0

A

perfect linear relationship
very strong linear
strong linear
moderate linera
weak linear
very weak linear
no linear relationship

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108
Q
  1. As part of the application for an Environmental Compliance Certificate (ECC), the Department
    of Environment and Natural Resources Administrative Order 2000-28 requires an additional
    requirement of producing an Engineering Geological and Geohazard Assessment Report
    (EGGAR) covering subdivision, housing, and other land development and infrastructure projects.
    Which of these events led to the creation of DAO 2000-28?
A

Cherry Hills Landslide in Rizal

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109
Q

A vector-based data structure is made for storing terrain information in digital terrain modeling
in which each sample point has an xy coordinate and a height, or z value. All the points are
connected by edges to form a network of non-overlapping triangles that collectively represent the
terrain surface. This network is known as

A

TIN

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110
Q

It is a mathematical operation defining the change of shape of a waveform resulting from its
passage through a filter.

A

convolution

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111
Q

. A correlation coefficient of ± .81 to ± 0.99 indicates _________ linear relationship

A

very strong

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112
Q

The Argyle Diamond Mine is the most significant source of pink diamonds in the world and is
located in Western Australia. The diamond deposit occurs in a ____________ pipe.

A

Lamproite

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113
Q

This surface feature is a liquefaction effect during an earthquake, characterized by fissuring
and buckling.

A

Lateral spreading

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114
Q
  1. Reporting of mineral resources is just one of the geologist’s roles in the profession. Which of
    the following classification has the best level of geological knowledge and confidence?
A

Measured

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115
Q

In hydrogeology, this term is applied in the search for groundwater, meaning a surface of
equal fluid pressure within the rock mass

A

Piezometric surface

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116
Q

The Mining Act of _____ (Commonwealth Act 137) introduced the Regalian Doctrine (lands &
minerals owned by the state)

A

1935

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117
Q

An oxide ore was observed in a porphyry copper deposit. It is an indication that the ore is at

A

Upper portion of the deposit

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118
Q

Orebodies formed by hydrothermal fluids and gases that were introduced into the host rocks from elsewhere, filling cavities in the host rock. describes mineral deposits formed later.

A

Epigenetic

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119
Q

ore deposits formed at the same time as the enclosing rock

A

syngenetic

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120
Q

a naturally occurring alloy of gold and silver, with trace amounts of copper and other metals

A

electrum

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121
Q

a rare cadmium bearing metal sulfide mineral consisting of cadmium sulfide (CdS) in crystalline form. Greenockite crystallizes in the hexagonal system

A

Greenockite

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122
Q

an analytical technique used to determine how much of certain elements are in a sample. It uses the principle that atoms (and ions) can absorb light at a specific, unique wavelength. When this specific wavelength of light is provided, the energy (light) is absorbed by the atom.
a technique for measuring the concentrations of metallic elements in different materials

A

Atomic absorption spectroscopy
AAS

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123
Q

alloy of iron with chromium and nickel.

A

Stainless steel

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124
Q

can be used in solar cells, which turn light energy into electrical energy.

A

Ruthenium

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125
Q

mainly used for research purposes.

A

scandium

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126
Q

Metallurgical process for dissolution of metals by means of acid solution. Examples include extraction of copper from oxide- or sulfide-bearing ore and dissolution of uranium from sandstone ores. Acid leaching can occur on heap-leach pads or in situ.

A

acid leaching

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127
Q

A colloquial term for petroleum

A

black gold

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128
Q

mark the upper and lower limits of normal variation for a particular population of data.

A

threshold values,

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129
Q

a 2-dimensional reference surface, to convert locations
from a curved surface to a flat surface

A

map projection

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130
Q

Started in 1953, this mine is the oldest porphyry copper mining operation
in the country

A

Atlas (Toledo)

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131
Q

Which coordinates could be the approximate geographic center of the
Philippines

A

o 13⁰N, 122⁰E

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132
Q

a bulk underground mining method, which allows large low-grade deposits to be mined underground. This method involves undermining the orebody to make it collapse under its own weight into a series of chambers from which the ore extracted.

A

block caving

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133
Q

trike-slip movements along the Philippine Fault and the Digdig Fault within the Philippine Fault System.

A

1991 luzon earthquake

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134
Q

seismically active regions in the country and has active faults that include the Masbate and Sibuyan Sea Segments of the Philippine Fault (PF), and potentially active faults that include the Uson Fault and Southern Masbate Fault.

A

2003 masbate earthquake

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135
Q

the movement of one of the Philippines’ largest fault; the Philippine Fault System with the focal mechanism corresponding to strike-slip.

A

ragay gulf earthquake

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136
Q

A “blind” gold-rich copper porphyry deposit was discovered in Surigao in
2000 at

A

Boyon- gan and Bayugo

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137
Q

clay of choice for degradable sulfur fertilizer.

A

Bentonite

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138
Q

toxic elements in mining?

A

cadmium, arsenic, lead, and mercury.

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139
Q

Involves recording core recovery and rock mass defects by RQD or Rock
Quality Determination, including other information on discontinuities and
structures (fault, fractures, bedding) recorded in the core

A

geotechnical logging

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140
Q

a zone around a mineral deposit where the metal values are less than those of the deposit but significantly higher than background values found in the country rocks around the deposit

A

dispersion halo

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141
Q

mass of ore deposited in a vein. consists of the most valuable part of the ore deposit.

A

oreshoot

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142
Q

A circular or crescentic distribution pattern about the source or origin of a mineral, ore, mineral association, or petrographic feature

A

mineralized halo

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143
Q

an electrochemical effect caused by many factors, not all of which are completely understood.

A

chargeability

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144
Q

The product of conductivity and thickness, typically measured in units of siemens

A

conductance

144
Q

an electromagnetic technique which assesses the ability of the topsoil or ploughsoil and features within it to be magnetised.

A

magnetic susceptibility

144
Q

atoms and particles move to new locations and geochemical environment

A

geochemical dispersion.

145
Q

an often produce a higher-grade commodity

A

deep narrow veins mining

145
Q

A method of mining in which large quantities of low-grade ore are mined without attempt to segregate the high-grade portions.

A

bulk mineable

146
Q

type of alteration system that has undergone advanced argillic and argillic alteration and is mainly composed of acid-sulfate alteration minerals characterized by alunite–kaolinite–dickite–quartz ± pyrite

A

lithocap

147
Q

non-ferromagnesian minerals.

A

Muscovite, Potassium Feldspar (Orthoclase), and Quartz:

148
Q

Fresh water -

Slightly saline water - Moderately saline
water -

A

Less than 1,000 ppm.
From 1,000 ppm to 3,000 ppm.
From 3,000 ppm to 10,000 ppm.

149
Q

This is a method of recovering gold and silver from pregnant cyanide
solutions by adsorbing the precious metals to granules of activated
carbon

A

activated carbon adsorption.

150
Q

anging between 1 and 4 μm.
Microcrystalline calcite, with a grain size finer than 4 μm;

A

Micrite,

151
Q

Limestone often contains larger crystals of calcite, ranging in size from 0.02 to 0.1 mm (0.79 to 3.94 mils)

A

sparry calcite or sparite.

152
Q

a pluton of igneous rock parallel to the bedding plane or foliation of folded country rock. More specifically, it is a typically lens-shaped pluton that occupies either the crest of an anticline or the trough of a syncline.

A

phacolith

153
Q

geological structure consisting of mobile material that was forced into more brittle surrounding rocks, usually by the upward flow of material from a parent stratum.

A

diapir

154
Q

a type of limestone that is composed of predominantly, more than 50 percent, of either clay-size or both silt-size and clay-size detrital (transported) carbonate grains.

A

calcilutile

155
Q

a ferro magnesian phyllosilicate mineral occurs as secondary in high temperature alteration zones in potassic altered porphyry copper deposits

A

biotite

156
Q

cryptocrystalline masses of apatite in phosphorite rich sed rock
referred to

A

collophane

157
Q

the sequence in which the minerals are formed in an ore deposit.

A

paragenesis

158
Q

Applied to dark-colored rocks, esp. igneous rocks, containing between 60% and 100% dark minerals;

A

melanochractic

159
Q

light-coloured because of a low content of ferromagnesian minerals.

A

leucocratic

160
Q

Neither leucocratic nor melanocratic; having a more or less even mixture of light and dark constituents.

A

mesocratic

161
Q

Bentonite clay is used as drilling mud, and mainly contains the mineral

A

60-80% of montmorillonite.

162
Q

The volcanic equivalent of an ultramafic rock

A

komatiite and picritic basalt

163
Q

most common titanium mineral?

A

Ilmenite

164
Q

minerals display one direction of well developed
cleavage

A

Biotite

165
Q

texture that is locally found in sphalerite in which unevenly distributed, variably sized blebs of chalcopyrite occur throughout a grain of sphalerite

A

Chalcopyrite disease

166
Q

A rock that is a mixture of metamorphic rock and igneous rock

A

migmatite

167
Q

If vesicles are so abundant that they make up over 50% of the rock and
the rock has a density greater than 1, then the rock is said to be

A

scoraceous.

168
Q

Where can a kelyphitic rim be found?

A

Where can a kelyphitic rim be found?

169
Q

Nacre is the layers of which a pearl is made of. What mineral is it

A

aragonite

170
Q

coarse crystalline calcite cement which fills pore spaces in many limestones after deposition, formed by the precipitation of calcite from carbonate-rich solutions passing through the pore spaces in the sediment

A

sparite

170
Q

The “alkaline” rocks typically are chemically undersaturated with respect
to

A

silica

170
Q

What was the name of the geoloist who first introduced the concept of
metamorphic facies?

A

Eskola

171
Q

When substantial chemical change accompanies metamorphism also called allochemical metamorphism

A

metasomatism’

172
Q

The term lamination is used for what thickness of bed?

A

less than 1cm

173
Q

the association of lath-shaped euhedral crystals of plagioclase, grouped radially or in an irregular mesh, with surrounding or interstitial large anhedral crystals of pyroxene;

A

ophitic texture

173
Q

refers to crystals, typically phenocrysts, in an igneous rock which contain small grains of other minerals.

A

poikilitic

174
Q

a texture of extrusive rocks in which the groundmass contains little volcanic glass and consists predominantly of minute tabular crystals, namely, sanidine microlites

A

trachytic

175
Q

What is measured by a goniometer?

A

interfacial angle

176
Q

a mineral deposit of gravel, sand, and nitrates, found especially in dry areas of South America

A

caliche

176
Q

very young soils with weak horizon differentiation;

A

Fluvisols

176
Q

determine the ages of formation and thermal histories of potassium-bearing rocks and minerals of igneous, metamorphic and sedimentary origin, as well as extraterrestrial meteorites and lunar rocks

A

K-Ar method

177
Q

a scientific method that can accurately determine the age of organic materials as old as approximately 60,000 years.

A

carbon 14 dating

177
Q

one of the oldest and most refined of the radiometric dating schemes.

A

u-pb method

177
Q

The long-term accumulation of sediment in a channel and the readjustment of the stream profile where there is a vertical growth of the land surface is called

A

Aggradation

177
Q

Removal of dissolved or suspended material from a layer or layers of the soil by the movement of water when rainfall exceeds evaporation.

A

eluviation

178
Q

The first fishes had no jaws, bones, only cartilages. Their
name means “shell-skins”, and these were called

A

ostracoderms

179
Q

The horizontal component or amount of dip separation,
perpendicular to the strike of the fault

A

Heave

180
Q

Element with an affinity for silicate phases

A

Lithophile elements

181
Q

“iron-loving”

A

siderophile

181
Q

found in, attracted to, or having a tendency to occur in the atmosphere. used especially of chemical elements or compounds.

A

atmophile

182
Q

This scientist discovered the P’ discontinuity, or the Pwave deflections at inner-outer core boundary

A

Inge Lehmann

182
Q

This
biozone type is a body of fossiliferous strata between
two specified biostratigraphic horizons

A

Interval zones

183
Q

The body of strata representing the known stratigraphic and geographic range of occurrence of a particular taxon or combination of two taxa of any rank.

A

Range Zone

184
Q

named for the taxon in the lineage whose range or partial range it represents

A

A lineage zone

185
Q

defined by the biohorizons across which there is notable change in the abundance of the specified taxon or taxa that characterize the zone.

A

abundacne zone

186
Q

The Indo-Australian plate is presently subducting under
the Eurasian Plate along the trench in Indonesia

A

Sumatra

187
Q

The study of trace fossils

A

ichnology

188
Q

branch of paleontology that deals with the processes of fossilization.

A

taphonomy

189
Q

the practice and science of categorization or classification.

A

taxonomy

190
Q

Lineated fault surfaces that have been polished by the
process of frictional sliding

A

Slickensides

191
Q

a series of relatively small, alternating, interlocked, toothlike columns of stone;

A

stylolite

191
Q

an imaginary sea level surface that undulates (has a wavy surface) over all of the earth; i

A

geoid

192
Q

Materials, especially rock masses, that formed in their present location and have not been transported. Fault surfaces can separate indigenous rocks from allochthonous rocks, although some allochthonous rocks are clearly delineated by their differing composition.

A

authochthonous

193
Q

convex upward ontaining progressively younger rocks from their core outwards are anticlines has a crest, which is the highest point on a given stratum along the top of the fold.

A

antiform

193
Q

objects have been displaced from their original site of origin

A

Allochthonous

193
Q

sediment of which at least 30 percent is composed of the skeletal remains of microscopic floating organisms. deposits of soft mud on the ocean floor.

A

ooze, pelagic

194
Q

the steepest line that can be drawn on an inclined plane. Measured in terms of inclination (from the horizontal) and its bearing (from north), and when used in conjunction with unit length it can be considered a vector quantity. The azimuth of the dip is at right angles to the strike of a bed.

A

true dip

195
Q

the angle between the horizontal and a planar or tabular geologic feature such as a bed, fault or vein as seen in a structure section. When the section is per- pendicular to the strike, apparent dip equals true dip;

A

apparent dip

196
Q

Which sedimentary basin is bounded by the Luzon
Central Cordillera and the Sierra Madre Ranges

A

Cagayan

197
Q

What type of coastline is formed during sea level rise

A

Submergent coastlines

198
Q

This Plio-Pleistocene Philippine fossil is considered to be
a sister group of the mammoth and elephants

A

Stegodon

199
Q

The opening and closing of ocean basins through plate
tectonics

A

Wilson Cycle

200
Q

A statement of elastic deformation, that strain is directly
proportional to stress

A

Hooke’s law

201
Q

The Palawan micro-continent collided with the Philippine
Mobile Belt during the

A

late Early Miocene to early Middle Miocene age (20-16 Ma)

202
Q

A tectonic process by which material is added to a
tectonic plate or a landmass

A

Accretion

203
Q

an act or instance of placing two elements close together or side by side

A

Juxtaposition

204
Q

The sediment that a stream moves along the bottom of
its channel by rolling and bouncing

A

Bedload

204
Q

The first period (542 to 488.3 Ma) of the Paleozoic Era,
during which most modern animal phyla developed

A

Cambrian Explosion of Animal Life

205
Q

Which of the following rocks could least or not preserve
fossils

A

sandstone

206
Q

Which rock formations could you find stream water that is considered “hard water”

A

limestone

207
Q

Which major plate consists entirely of oceanic
lithosphere

A

Pacific

208
Q

In geologic time, when could be the beginning of the
Phanerozoic Eon

A

541

209
Q

dinosaurs diversified
and the first birds appeared

A

Late Cretaceous

210
Q

A basin that forms on the side of a volcanic arc away
from the trench

A

back arc

211
Q

Zone of saturation; area in aquifer, below the water
table, which relatively pores/fractures are water
saturated

A

phreatic zone, saturated zone, or zone of saturation

212
Q

The dome-shaped top of an igneous intrusion

A

cupola

213
Q

The lowest point of a ridge connecting two mountain
peaks, often constituting a pass or a saddle

A

col

214
Q

The angle that a bedding plane or fault makes with the
horizontal

A

dip

215
Q

provides a direction given as the primary compass direction (north or south), degree of angle, and an east or west designation. A bearing describes a line as heading north or south, and deflected some number of degrees toward the east or west.

A

bearing

216
Q

the angle between North, measured clockwise around the observer’s horizon, and a celestial body (sun, moon)

A

azimuth

217
Q

also termed the unsaturated zone, is the part of Earth between the land surface and the top of the phreatic zone, the position at which the groundwater is at atmospheric pressure

A

vadose

218
Q

The stress exerted by the water present in the soil pores

A

pore water pressure

219
Q

energy per unit weight of fluid is termed as

A

head

220
Q

common mineral that replaces organic substances in fossil formation

A

SiO2

221
Q

niagara falls has a limestone cap underlaid by

A

granite

222
Q

feature below that is most useful in indicating the direction of movement of continental glacier

A

drumlin

222
Q

sinkhole lakes would be found most readily in?

A

florida

223
Q

the most recent covering of New England by continental glaciers ended at a time closes to which one of the following

A

10,000 BC

224
Q

earliest deposits of graphite left by simple forms of life resulted from such life in

A

archeozoic

225
Q

the study of radioactive minerals shows the earth to have a minimum age in years closest to

A

5,000,000,000

226
Q

minimum average monthly temperature required for a zone to be considered tropical

A

64 degrees Farenheit

227
Q

information about auroras

A

occur near the poles only
are caused by ionization of oxygen and nitrogen in the upper air
at their brightest during maximum sunspot activity

228
Q

closest distance in miles from the Earth to the moon

A

2.5 x 10 ^5

229
Q

a plane on a great circe route

A

a meridian

230
Q

not truly described by its name

A

sea

231
Q

boothbay maine is charac by

A

long narrow bays

232
Q

deflecting force of ferell cell is greatest at what

A

80 degrees N

233
Q

one known 20th century for its most violently explosive type of eruption

A

mt.pelee martinique

234
Q

star nearest to the sun is in the constellation

A

centaurus

235
Q

summer solstice the vertical rays of the sun at noon are on the

A

tropic of cancer

236
Q

a mature river will become intrenched when the area in which it is located is

A

elevated

237
Q

gently undulating, almost featureless plain that, in principle, would be produced by fluvial erosion that would, in the course of geologic time, reduce the land almost to baselevel (sea level), leaving so little gradient that essentially no more erosion could occur.

A

peneplain,

238
Q

fall lines cities are located where rivers flow from the rocks of

A

older Appalachians to those of the coastal plain

239
Q

most cenozoic mammal fossils were preserved by

A

burail after drowning or suffocation

240
Q

skull of pithecanthroupus erectus differs from other ape why?

A

lack of median crest

241
Q

one in which the greatest variety of species is found in

A

cenozoic protozoa

242
Q

the triangulation point on a tropographic map

A

true elevation

243
Q

a heavy black line on a geologic map with the letters U and D appearing on opposite sides of the line

A

fault

244
Q

the symbol T 30 indicates

A

dip E-W strike 30 degrees N

245
Q

a sequence of sedimentary rock layers that progress from deep-water and turbidity flow deposits to shallow-water shales and sandstones. It is deposited when a deep basin forms rapidly on the continental side of a mountain building episode.
consists of repeated sedimentary cycles with upwards fining of the sediments. There are sometimes coarse conglomerates or breccias at the bottom of each cycle, which gradually evolve upwards into sandstone and shale/mudstone. ypically deposited during an early stage of the orogenesis. When the orogen evolves, the foreland basin becomes shallower and molasse is deposited on top of the flysch.

A

Flysch

246
Q

These deposits are typically the non-marine alluvial and fluvial sediments of lowlands, as compared to deep-water flysch sediments.

A

Flysch and Molasse

246
Q

refers to sandstones, shales and conglomerates that form as terrestrial or shallow marine deposits in front of rising mountain chains. The molasse deposits accumulate in a foreland basin, especially on top of flysch-like deposits.

A

“molasse”

247
Q

semi-precious stones include

A

ambales Jade” (uvarovite) and mauve, “Mindoro Jade” (sericite schists), minor floats of jadeite and nephrite, jasper/chert, serpentine, spinel, garnet, quartz, epidote, obsidian, bloodstone, agate, opal, tektite, azurite, malachite, amber, corals, and pearl considered as the National Gem of the Philippines.

247
Q

s a reaction where a solid phase and liquid phase will together form a second solid phase at a particular temperature and composition

A

Peritectic

247
Q

ormed by self-generated alteration of a granite and is a class of endoskarn; It means that greisen in most cases formed inside the granitic pluton itself that provided heat and hydrothermal fluids to initiate the greisenization.
commonly, are granitoid rocks in which >90% of the feldspar is replaced by quartz, mica, topaz, cassiterite and other minerals.
Commonly hosts workable - though not always currently economic - Sn - W - Mo ore bodies

A

Greisen

247
Q

Some deposits of these semi-precious stones are in:

A

Sta. Cruz, Zambales; Sta. Cruz, Occidental Mindoro; San Vicente- Mabini-Dasol, Pangasinan; Burgos, Ilocos Norte; Paracale, Camarines Norte; and Nagcarlan, Laguna.

248
Q

what are the zeolite minerals

A

natrolite
analcime
laumontite
chabazite
clinoptilolite
heulandite
stilbite
sodalite

248
Q

what are under incohesive non-foliated and foliated

A

non-foliated: fault breccia >30%visible fragments
fault gouge <30% visible fragments

foliated
foliated gouge

248
Q

equant with a nearly square cross sections halite galena

A

blocky

248
Q

what are under the cohesive non foliated

A

pseudotachylyte
crush breccia- fragments>5mm
fine crush breccia- fragmants 1-5mm
crush microbreccia fragments <1mm

catacalsites grain size reduction by cataclastic mechanisms

protocataclasite
cataclasite
ultracataclasite

249
Q

under cohesive foliated

A

mylonite series
grain size reduction by plastic def mechanism
protomylonite
mylonite
ultramylonite

grain size increase by recrystallize
blastomylonite

249
Q

Microcrystalline rocks of granitic composition

A

Felsite

250
Q

gneous rock texture in which an intergrowth of two minerals has the appearance of runic writing. Graphic textures are most commonly intergrowths of quartz and alkali feldspar in which the quartz appears as v-shaped inclusions enclosed by the feldspar.

A

Graphic Granite

250
Q

An opaline sinter that is often found around hot springs and geysers. A botryoidal form is called fiorite.

A

Geyserite

250
Q

form from waters that separate from a magma in the late stages of crystallization; this activity often occurs in small pockets along the margins of a batholith. Pegmatite can also form in fractures that develop on the margins of the batholith.

A

Pegmatites

250
Q

also made of silica, but tufa and travertine are made of calcium carbonate.

A

Diatomite

251
Q

general term for sandstone. It is equivalent to the Latin-derived term arenite and is commonly used in various publications to describe a metamorphosed sedimentary rock with a dominantly sandstone protolith

A

Psammite

251
Q

coarse gravel
medium sand
fine clay

A

psephite rudite
psammite arenite
pelite lutite

252
Q

a=b=c all angles 90 degrees

A

cubic fluorite

253
Q

a=b not equal to c
all angles at 90

A

tetragonal rutile

254
Q

a=b not equal to c
angles 120 or 90

A

hexagonal beryl

255
Q

abc all not equal all angles 90

A

orthorhombic
enstatite

256
Q

all abc not equal
a=y=90
beta not equal 90

A

monoclinic sanidine

257
Q

abc not equal and no angles 90

A

triclinic albite

258
Q

along with minerals of the melilite group, are referred to as foids in the IUGS classification of igneous rocks. They do not occur in igneous rocks containing original free silica. They are, in fact, incompatible with quartz, as is quite apparent from the following equations:

nepheline +quartz=albite and leucite+ quartz= k felds

A

Feldspathoids

259
Q

A coarse-grained crystalline rock consisting mostly of calcic plagioclase (>90%, usually labradorite) with <10% mafics. The lunar highlands are composed predominantly

A

Anorthosite
Because of linguistic similarities some people think that anorthosite is a rock composed of anorthite (one of plagioclase group minerals). This is not true. Anorthosite is usually composed of labradorite and sometimes bytownite or andesine as well (all plagioclase group minerals).

260
Q

main factor that detemines the texture of an igneous rock is

A

cooling rate dT/dt

261
Q

rate at which atoms or molecules can move through the liquid

A

diffusion rate

262
Q

rate at which enough of the chemicla constituents of a crystal can come together in one place w/o dissolving

A

rate of nucleation of new crystals

263
Q

the rate at which new constituents can arrive at the surface of the growing crystals depends largely on the diffusion rate of the molecules of concern

A

rate of growth of crystals

264
Q

small degrees undercooling the nucleation rate will be low and growth rate moderate since few nuclei

A

phaneritic texture

265
Q

larger degrees of undercoolingnucleation rate will be high and the growth rate also high

A

aphanitic

266
Q

hugh degrees of undercooling both the growth rate and nucleation rate will be low few crystals will form and they will not grow to any large size= glassy

A

holohyaline texture

267
Q

small holes left behind after lava cools and turns into volcanic rock. help geologists understand the cooling history of extrusive (volcanic rocks) because lava contains large amounts of dissolved gases that are released as the lava hardens.

A

vesicular

268
Q

if phenocrysts are found to occur as clusters of crystals then the rock should be described as glomeroporphyritic instead of porphyritic

A

glomeroporphyritic

269
Q

if vesicles have been filled with material usually calcite chalcedonyor quartz then the term amygdularshould be added to the textureal desciption of the rock defined as a refilled vesicle

A

amygdular

270
Q

vesicles are so abundant that they make up over 50% of the rock and the rock has a density less than 1 would float inwwater then the rock is

A

pumiceous

271
Q

vesicles are so abundant that they make up over 50% of the rock and the rock has a density greater than 1 then the rock is

A

scoraceous

272
Q

texture consisting of intergrowths of quartz and alkali feldspar wherein the orientation of the quartz grains resembles cuneiform writing most observed in pegmatites

A

graphic

273
Q

texture commonly found in glassy rhyolites wherein spherical intergrowths of radiating quartz and feldspar replace glass as a result of devritification

A

spherulitic

274
Q

texture usually restricted to coarser grained rocks that consists of concentrically banded spheres wherein the bands consist of alternation light colored and dark colored minerals

A

obicular

275
Q

fine
medium
coarse
very coarse

A

<1mm diameter <sugar granules
1-5mm diameter (sugar to pea sized)
5-50mm diameter
>50 mm diameter lower size limit is not really well defined

276
Q

When basaltic lava flows enter standing water, they form either tongues or more
equidimensional blob-like structures, both of which are called pillows. The resulting pillow
lavas contain numerous packed pillows, usually with glassy rinds, concentric
bands, and radial fractures within. Later pillows commonly flatten and conform to the shape of
the pillows upon which they settle, providing geologists with a method of determining the
original top of the deposit in folded terranes. The
hyaloclastite commonly devitrifies quickly to an orangish- brown material called

A

Palagonite

277
Q

The pillows may be embedded in fine glassy debris
called

A

hyaloclastite

278
Q

0.25-2.5km diameter

A

scoria cone

279
Q

0.2-3.0km diameter

A

maar

280
Q

0.2-3.0km diameter

A

tuff ring

281
Q

0.1-1.5 km diameter

A

tuff cone

282
Q

eskola proposed this diagram a way to illustrate metamorphic mineral assemblages on a simplified 3-componetn triangular diagram. He concentrated only on the minerals that appeared or disappeared during metamorphism thus acting as indicators of metamorphic minerals

A

ACF Diagram

283
Q

the norm is a method of recalculating a chemical analysis of an igneous rock into a set of ideal minerals. the norm was originally proposed as a method of classifying igneous rocks but the classification has since given way to drect chemical classifications. the norm is still used by some petrologists and it is most useful for volcanic or glassy rocks where the modal mineralogy is unavailbel. in the US commonl use formaulation developed by COPW which expresses the normative mienrals as weight percentages. the method descrived here is a simplication norm which expresses the normative minerasl as molecular percentages. the following mid ridge ocean basalt analysis will be usead as an illustration of the techniqua.

A

CIPW cross iddings pirsson and washington

284
Q

a hypothesis-testing paradigm for the evaluation of rock geochemistry, and generally provides an understanding of the nature and extent of material transfer that has taken place in a suite of rocks.

A

Pearce element ratio (PER)

285
Q

zeolites especially laumontite,wairakite,analcime in place of other Ca-Al silicates such as phrenite,pumpellyite,and epidote

A

zeolite

286
Q

phrenite,pumpellyite, +chlorite + albite

A

phrenite,pumpellyite,

287
Q

chlorite+albite+epidote(zoisite) +actinolite+quartz

A

greenschist

288
Q

hornblende+plagioclase (oligoclase,andesine)+garnet

A

amphibolite

289
Q

orthopyrozene+clinopyroxene+plag+garnet

A

granulite

290
Q

glaucophane+lawsonite or epidote/zoisoite+ albite +chlorite+garnet

A

blueschist

291
Q

pyralpsite garnet+omphacitic pyroxene+kyanite+quartz no plagioclase

A

eclogite

292
Q

mineral assembalges in mafic rocks of the facies of contact metamorphism do not differ substantially from those of the corresponfing regional at higher pressure

A

contact facies

293
Q

very low pressures

A

contact facies

294
Q

low pressure regional

A

buchan or abukuma facies

295
Q

medium pressure regional

A

barrovian facies

296
Q

high pressure moderate temperature

A

sanbagawa facies

297
Q

high pressure moderate temperature

A

franciscan facies

298
Q

which one large crystal encloses many smaller crystals similar to ophitic textures but the enclosing mineral need no be pyrozene greenvile maine
6mm

A

poikilitic texture

299
Q

quartz wedge

A

530 nm plate 1/4 plate

300
Q

acute bisectriz is Z

A

positive

301
Q

acute bisectrix is X

A

negative

302
Q

angle between the optic axes bisected by the X axis as 2Vx and the angle between the optic axes bisected by the Z axis as 2Vz the angles then can vary between 0 and 180 degrees with restrcition that 2Vx+2Vz=180

A

if 2V is exactly 90 then neutral

303
Q

2V <90, 2Vx>90

A

positive

304
Q

2V>90, 2V<90

A

negative

305
Q

a property closely related to crystal shape, includes shape and size of crystal faces, how forms combine, how well developed different forms are, and the way multiple crystals grow together. Habit, thus, is the characteristic appearance a mineral can have. The photos in Figure 3.16 show some contrasting examples.

The most useful terms describing habit are self-explanatory. Common ones used to describe the habit of single crystals include equant (equidimensional), acicular (needlelike), tabular, and bladed. These and other terms are defined below.

A

habit

306
Q
A
307
Q

shows orange chabazite crystals on top of heulandite. Both of these are zeolite minerals that occur most commonly in openings within basalt, and less commonly in metamorphic rocks or hydrothermal veins. This sample comes from a classic locality near Wasson Bluff, on the shore of the Bay of Fundy, Nova Scotia, where many outcrops of 200-million year old basalt contain cavities filled with spectacular mineral specimens.

Although zeolites are best known for their occurrences in vugs and other open cavities in volcanic rocks, large volumes are found in volcanic ashes and saline lake deposits. Zeolites also may be present as products of diagenesis or low-grade metamorphism in sediments and rocks.

A

he zeolite group includes more than 40 minerals. They are, essentially, hydrated feldspars and are framework silicates containing open cavities that can hold loosely bonded large cations and water. The best-known use for zeolites is in water softeners. Because calcium in water causes it to be hard, suppressing the effects of soap, forming scale, or creating other problems, it is often filtered through zeolite. Zeolite charged with sodium ions (generally from dissolved salt) allows water to pass through its structure while exchanging calcium for sodium, thus making the water less hard. This process is reversible, so the zeolite can be flushed and used again.

308
Q

s a triclinic K-feldspar and has a characteristic cross-hatched tartan pattern of twinning seen with a petrographic microscope ad ample amount of time to cool down .

A

Microcline

309
Q

re both optically monoclinic K-feldspars. Sanidine occurs in volcanic and subvolcanic rocks. Orthoclase occurs in plutonic rocks.

A

Orthoclase and sanidine

310
Q

is a K-feldspar produced by low-temperature hydrothermal (veins) or authigenic processes. It is structurally similar to microcline but without the cross-hatched twinning. Low-temperature feldspars either crystallized at lower temperatures

A

Adularia

311
Q

the only alkali feldspar that is not K-feldspar. It is sodic in composition, optically triclinic and characterized by a twinning similar to microcline but on a smaller scale.

A

Anorthoclase

312
Q

igh temperature ordering because the cooling is very rapid

A

sanidine

313
Q

ault-related rock that maintained primary cohesion during deformation, with matrix comprising greater than 10 % of rock mass; matrix is fine-grained material formed through grain size reduction. Cataclasites are subdivided into those that have 10-50% matrix (protocataclasite), 50-90% matrix (cataclasite) and > 90% matrix (ultracataclasite).

A

Cataclasite

314
Q

are usually found in faults, which have been active at shallow crustal levels. They occur in fault zones of variable thickness and can be subdivided into

A

Incohesive brittle fault rocks

315
Q

n unconsolidated fault rock consisting of less than 30% matrix. If the matrix fragment ratio is higher, the rock is called a fault gouge. A fault gouge is thus a strongly ground-down version of the original rock. These unconsolidated fault rocks form in the upper part of the brittle crust. They are conduits of fluid flow in non-porous rocks but contribute to fault sealing in faulted porous rocks.

A

Fault breccia

316
Q

an be subdivided into cohesive breccia, cohesive cataclasite and pseudotachylyte. Cohesive cataclasite and breccia commonly show evidence for abundant pressure solution and precipitation effects. Rock fragments are transected by healed cracks aligned with fluid inclusions. Veins of quartz, calcite, epidote or chlorite, and in ultramafic rocks, serpentine, are common. These veins form during and after brittle deformation, since they have commonly been fractured.

A

Cohesive fault rocks

317
Q

oldest microscope national optics

A

then leica then recent is nikon

318
Q

Nikon microscope (as well as the Leica microscope) also have digital cameras attached to them, making them larger. The Nikon camera system includes the box sitting on the table to the right of the microscope.

These examples of National and Leica microscopes are student microscopes. The Nikon microscope shown here is a research-grade microscope. Please note that these companies each make different types and grades of microscopes: these are simply the examples we had at hand!

A

s a steady light source that is located in the base of the microscope. It is used for transmitted light microscopy.

The switch to turn on the illuminator is typically located at the rear or on the side of the base of the microscope. When the illuminator is ON, light will be visible through the base in the microscope. The following video clips show examples of turning on the illuminator for different microscopes:
illuminator

319
Q

The parts of the microscope that are located above the base but below the stage are called the

A

substage assembly. The substage assembly includes the condenser, the lower polarizer, light filters, and diaphragms.

320
Q

consists of two or more lenses that focus the illuminator light onto the sample placed on the stage, and one or more apertures to control illumination (see below). The condenser should be adjusted each time the objective lens is changed to maximize the quality of the image

A

condenser

321
Q

alogen lights used in microscopes typically give off a yellowish light, so a blue filter is often added to compensate for the yellow color of the light, providing a truer white light to pass through the sample.

A

A diaphragm or aperture cuts down the amount of light that reaches the sample by restricting the area that light can pass through. There are often multiple apertures on a microscope (Figure 2.4.5), including an aperture as part of the condenser assembly, as well as a field diaphragm that controls the size of the area which is illuminated on a sample

322
Q

The mechanical stage is an accessory which can be attached to the top of the rotating stage. Rather than a rotating motion, it allows motion along the x-axis (left-right) and y-axis (top-bottom). In Figure 2.4.10, the gold knob at the top controls motion in the x direction, and the gold knob on the right controls the y direction motion. The pincer-like arms (bottom left) wrap around the thin section and hold it in place.

A

Most polarizing light microscopes have two focusing knobs on each side of the microscope. The coarse focus is used to rapidly change the level of the stage and sample, and the fine focus knob is used to gently bring a sample into complete focus.

323
Q

Objectives are the main (but usually not the only) magnification mechanism in the microscope. Magnifications typically range from about 4x-64x, although objectives as low as 2.5x and as high as 200x are available. Because most polarizing light microscopes are compound microscopes containing more than one lens, the total magnification can be much higher (see the oculars section below).

A

The Amici-Bertrand lens (or simply the Bertrand lens) changes the plane of focus so that the viewer can observe interference figures

324
Q

he 1/4λ plate can also be called a mica plate, glimmer plate, or 147 nm.

A

yea

325
Q

Common Fluorescent Minerals
Over 500 minerals have been discovered that exhibit some sort of fluorescence when exposed to ultra violet light. What follows, is a collection of some of the more common and/or well-known fluorescent minerals. Importantly, not all specimens of these minerals will fluoresce, as minerals typically require an ion actuator to glow.

A

fluorite fluorospar
calcite
agrellite
apatite
aragonite
baryte
cerussite
Chalcedony
Corundum
Esperite
Hardystonite
Hyalite
Hydrozincite
Opal
Pyromorphite
Scapolite
Scheelite TUNSTEN
Selenite HOURGLASS
Smithsonite
Sodalite
Sphalerite
Tremolite
Tugtupite
Willemite
Wollastonite
Caliche

326
Q

lectron returns to its ground state (where it started) and releases the amount of energy it absorbed (thus returns light with that wavelength to the spectrum, thus, no color….

A

luminescence

327
Q

If some of the adsorbed energy is lost but the reminder is returned to the visible spectrum, the light returned has lower energy and thus, different color. [changes in energy = changes in wavelength = changes in color].

A

fluorescence

328
Q

are elements (e.g., Ti, V, Cr, Mn, Fe, Co, Ni, Cu…) that are not present in the pure compound. Impurities are elements that occur in low concentration in the gemstone.

A

Impurities

329
Q

Beryl containing iron (Fe):

Aquamarine = Fe++, beryl is blue
Heliodor = Fe+++, yellow
Green beryl : due to mixtures of Fe2+ and Fe3+
Beryl containing Manganese(Mn):
Morganite : Mn++ is pink
Red beryl : Mn+++ is red

A

Beryl containing Chromium(Cr):
Emerald = emerald green : Cr+++