Study Guide Test 2 Flashcards
Magma Differentiation
process that changes magma’s chemistry towards a more felsic composition over time
fractionation and assimilation
Fractionation
Magma composition erodes as mienrals crystallize out- remaining melt becomes silica rich and felsic
mafic to felsic
Burial Meta
Rock deeply buried 7200 m
Deep sedimentary basins
Extension of diageneis
Increasing temp, CONFINING pressure at depth- low grade- zeolic facus
Quartz sandstone- quartzite
Pegmatitic
very slow crystallization
Bedding Planes
Sedimentary material or deposition in horizontal layers forming beds
Beds are bigger than 1 cm thick
Defined by differene in color, sediment size, and/or resistance to erosion
A different bed incidactes change in sediment deposition conditions
texture
crystal grain size
Magma compositions of Calderas
Intermediate to felsic comp
Chemical Sedimentary rocks classification
organic
inorganic
biochemical
Inorganic Sedimentary- Banded Ions Formations
iron oxide precipitated from ocean water depositing on ocean floor in concentration bands, alternating with chert
Pressure Solution
Material is dissolved from highly stressed edges of grains
Styolid- pressure solution streams
Inorganic Sedimentary Rocks - Inorganic Chert
Microcrysyalline quartz precipitated out of silica rich groundwater
Jasper, Flint, Onyx, Agate
Fossiliferous limestone
abundant visible fossiles (marine invertebrates)
Coral reefs, shallow ocean setting, lakes
How does crystal size and metamorphic fabric (foliation degree) relate to metamorphic grade?
Smaller crystal size- low
Bigger crystal size- high
Foliation- high
Non-foliation- low
Rotation
Elongated and platy minerals can rotate so they become almost parallel to one another
Minerals that crystallize or grow in the differential stress field can have a preferred orientation
Schistosity- mica and other minerls with dominant orientation
Coal
large quantities of plant debris in wetlands/swamplands decays to peat and alters into an organic sedimentary rock
Order of Bowen’s reaction series
Ultramafic, Mafic, Intermediate, Felsic
Igneous Dikes
intrustion that cuts across the layer
vertical
6 different types of volcanoes
Cinder/Scoria Cones
Shield Volcanoes
Stratovolcanoes
Lava Domes
Calderas
Flood Basalts
Foliation Texture
A planer alignment of minerals and textures within a rock
Line on plane with no common direction
what controls magma viscosity
Magma Composition and temperature
compaction
pressure of overlying sediments decrease pore space between the grain
A sedimentary rock which contains environmental clues, such as grey-green mudstones with laminations and freshwater fossils, would mostly likely indicate which depositional environment?
lacustrine (lake)
Magma compositions of Flood Basalts
low viscosity
Basalt lava flows
Volcanic Hazards
Gases
Tephra
Pyroclastic Flow
lahar
Landslide
Tsunamis
Hot Spot has what type of igneous rock comp
oceanic- mafic to intermediate
continetal- mafic to felsic
Which statement is INCORRECT about Peridotite?
It is composed of an abundance of feldspar and quartz minerals.
Heat induced Melting
INCREASE in temp
melting of surrounding rocks from magma intruction of rising mantle plume
MANTLE PLUME
HOTSPOT
In what environments does low pressure/high temperature metamorphism occur
near magma intrustion at shallow depth
Mudstone
general term for fine grained sedimentary rocks
Transgressions
Rise of sea level and submergence of the continent under seawater
Depositional environments shift landwards (go further towards land, ocean expanding)
Difference between metamorphic texture and igneous texture
Metamorphic-
Descriptin of mineral grain shapes and orientation
Foliated or nonfoliated- granular, equi distance
Line up or not
Igneous
based on grain size and other features
cooling rate big influence
magma textures
Continental Subduction has what type of igneous rock comp
Ultramafic rock
mafic melt
Effusive Eruption
Non-explosive eruptions
low gas and low viscosity
lava dome and lava flow
Deltas
Transitional - Where rivers enters oceans
Three types- river delta, wave delta, tide dominated delta
Main sediment: channelized sand, mud, organic matter (swamp)
Main rock- clastic rocks, coal/organic sedimentary rocks (swamps)
Main structure- cross bed, delta seidments, sequence (muds to fine sand to coarse sands and organic rich rocks)
Main fossils- many to few fossils
What is incorrect about Batholiths
Most mafic in comp
How is temperature and pressure involved in metamorphism?
Temperature
Heat driven metamorphism occurs at 200 and continues until 700-1100
Pressure
Force exerted over an area, stress= applied force
Strain is product of stress/metamorphic dchanges within minerals
What are two things that influence initial magma compositions
Source of rock
degree of partial melting
True/False
Occasionally fine-grained sediments of the abyssal plane near continental slopes can contain courser sand-sized sediment carried by submarine landslides called turbidite deposits.
true
metamorphic grade
range of metamorphic change a rock undergoes, progressing from low (little metamorphic change) grade to high (significant metamorphic change) grade.
What does grain size, sorting, and clast shape indicate and environemtn distance
grain size- as size gets smaller, longer transport time
sorting- more well sorted the rock is, longer the distance
shape- rounder (smoother) it is, the longer the distacance
Shearing
Shear stress causes objects to be smeared out in the direction of applies stress
Augens- eye shaped
Bioturbation
Reworking of soft sediment by burrowing organisms
SHALLOW MARINE environments
Used to indicate WATER DEPTH
why are caldera, flood basalts, volcanic dome, stratovolcano more dangerous than scoria or shield
Scoria and Shielf- localized eruptions
Others- explosive eruptions that are far reaching
Composition
what minerals are present
Clastic Sedimentary rocks classification
Breccia
conglomerates
sandstones
mudstone
shale
Dunes
Meter Scale Ripples
Igneous rocks are classified based on which
texture
composition
True or False:
The presence of pillow basalts indicate lava flowed within a body of water.
true
Assimilation
incorporates the host rock that magma is intruding into
piece of surrounding block gets added to melt/magma, pieces partially melt
Contact meta
High temp low pressure
Local, small instruction
Shallow depth
Produce NON-FOLIATED rocks
Heat from magma alters rok in comes in contact with (heating, NO deformation)
What metamorphic rocks are diagnostic of subduction metamorphism?
Greenstone, greenschist, blueschist, eclogice
Inorganic Sedimentary rocks- rich groundwater
abundant dissolved ions precipiate out of solution-
lakes streams hot spring, caves
stalagmaite and stalactite
Physical processes metamorphism
Deformation of objects
Rotation
Shearing
Ultramafic
Mantle rocks
Contains MOST of Fe, Mg, and Ca
LEAST amount of silica
Periodite- intrusive
Kmoatite- Extrusive
Biochemical
formed from shells/skeletons of marine/freshwater organisms
Organisms extract dissolved material out of water to form shells, when dies, the hard parts deposit on sea floor as sediment that lithifies when buried
fossiliferous limestone
chalk
biogenic chert
stromatolites
true/false
The metamorphic rock, mylonites, are associated with fault metamorphism where fault shearing occurs at deeper depths.
true
Why does contact metamorphism produce only non-foliated metamorphic rocks?
No pressure that foliated one need
Inorganic Sedimentary rocks high evaporation rate
cause bodies of water to dry up
Dissolved ions precipitation out of solution
Forming evaporate minerals
Salt, calcite, gypsum, halite
Three ways magma can form
Decompression Melting
Flux Melting
Heat Induced Melting
Partial Melting
different minerals make up rocks, minerals melt at different times
Resulting melt more felsic
increase from ultramafic to mafic- felsic melts from rock sooner
Lacustrine
Continental- Lakes
Low energy environment
Main sediment- fine-grained
Main rock- shale
Main structure- lamination
Main fossil- freshwater organisms
Tephra
ash
explosive eruption produce it and the wind carry it long distances
WIth enough- collapse buildings, cause Silicosis (respiratory issues)
Explosive Pyroclastic Eruption
Explosive eruption
high gas and high viscosity
lava fountaining, pyroclastic flow, eruption channel + ash cloud
Pyroclastic Flow
fast flow of lava blocks, pumice, ash, and hot gases
collapse of eruption column or lava dome
MOST DANGEROUS
STRATOVOLCANO or LAVA DOME
what gives igneous rocks fine grained, aphanitic texture
When a lava has a fast cooling rate,
Biological Activity
Root wedging- plant roots work themselves into cracks, prying the bedrock apart as they grow
tunneling organisms like earthworms, termites, and ants
Graded Bedding
Change in grain size within a sediment bed
Trends from coarse to finer; or finer to coarser
Caused by changes in currents speed
Events like FLOOD, LANDSLIDES, SUBMARINE LANDSLIDES
Fault Meta
Fault where reach duxtile zone- shear rock
Mylongic form- created by dynamic recrystallization through directed shear forces
Larger, stronger mineral crystals may form augments
Magma compositions of shield volcanoes
low viscous
mafic magma chambers
Chemical weathering
water, oxygen, and other reactants chemically degrade the mineral components of bedrock
protolith for quartzite
quartz rich sandstone
what is relationship between cooling rate and igneous rock type
extrusive- faster cooling
intrusive- slower cooling
relationship between cooling rate and mineral crystal size (igneous)
faster cooling rate means smaller crystal size
slower cooling means larger crystal size
Oxidation
chemical reaction with oxygen causing rusting metallic iron
iron minerals bond with oxide minerals, exposed to Earth’s atmosphere
Vesicles- what does it indicate
pressure gas bubbles
magma is gassy- explosive
Slate-phyllite-schist-gneiss sequence
Sandstone
sand lithified to sandstone
coarse grains
wide variety of mineral grains
grain roundness varies
moderate to well sorted
Physical appearance of Flood Basalts
large igneous provinces
multiple explosive centers from fissured dikes
Low viscosity
lava spreaf out- higher temp and FEWER silica chains (mafic)
What does low vs high grade metamorphism indicate?
Low – finer grained crystals
High- coarser grained crystals
What are the differences between regional, contact, and subduction metamorphism?
Regional
Increasing temperature and Pressure
Heating AND deformation
Foliated
Range of depth
Contact
High temp, low Pressure
Heating NO deformation
Non-foliated
Shallow depth
Subduction
High Pressure low temp
Deformation NO heating
Dissolution
some minerals completely dissolve when reacting with water and natural acid
produce dissolved ions in water
followed by precipiation and often focused in fractures
As magma cools minerals crystallize out causing a change in the remaining magma composition. What is this process called?
Fractional crystallization
Metamorphic textures
foliation
lineation
non-foliated
schistosity
Which is NOT commonly associated with lava domes, stratovolcanoes, and calderas?
Mafic- Intermediate lava comp
Shield volcanoes have low slopes primarily because
the low viscosity of basaltic magma allows it to flow downhill for long distances.
How does fluids play a role in metamorphism
Interact chemically with minerals and cause new mienrals to replace existing ones
Hydrothermal metamorphic alteration
Can remove elements from rocks- seawater flows through fractures in fresh, hot basalt, reacting with and removing mineral ions
What does presence of coarser vs finer clast size indicate about energy of envionment and distance
coarser- high energy- small distance
finer- low energy- long distance
When material from a subducting slab reaches a certain depth, what gets released and added to the mantle above to cause the mantle to melt?
H2O
water
Inorganic Sedimentary Rock- Travertine
calcite slowly precipitate from water, leaving thin band/layer (caves and hot spring)