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77 Cards in this Set

  • Front
  • Back

Type: Metamorphic


Name: Slate


Texture: Slaty cleavage


Foliated: Yes


Other: Relict bedding


Position: Forearc Basin - Sediment carried off shore become concentrated here. Land derived character of the sediments is evident in the nature of the fossil compartments preserved in the shale (e.g. Light weight plant debris swept out to sea by floods)

Type: Metamorphic


Foliated: Yes


Name: Granulite


Texture: Gneissic foliation


Mineralogy: feldspar, plagioclase, quartz


Position: Volcanic arc

Type: Metamorphic


Foliated: Yes


Name: Schist


Minerals: Muscovite, biotite, staurolite, andalusite, chlorite, quartz


Texture: Schistose foliation


Other: Garnet porphyroblasts


Position: Frontal arc?

Type: Metamorphic


Foliated: No


Name: Quartzite


Texture: Granoblastic


Minerals: Calculate, Dolomite, Quartz


Other: Relict bedding, interlocking quartz grains

Type: Metamorphic


Foliated: Yes


Texture: Schistose


Minerals: Staurolite, Chlorite


Other: Porphyroblasts of staurolite


Name: Schist



Type: Metamorphic


Foliated: No


Texture: Granoblastic


Minerals: Calcite, Garnet, Diopside


Other: minerals clumped by composition


Name: Skarn (York River Specimen)

Type: Metamorphic


Foliated: Yes


Texture: Phyllitic


Other: Silky/satin sheen, fine grained


Name: Phyllite

Type: Metamorphic


Foliated: No


Minerals: Jasper, hematite, magnetite


Others: Relict bedding, folding


Name: MetaBIF

Type: Metamorphic


Foliated: Yes


Texture: Mylonitic


Minerals: quartz


Others: Flattened porphyroclasts in fine grained groundmass


Name: Mylonite

Name: Granulite


Age period: Permian

Name: Quartzite

Name: Skarn

Name: Hornfels

Name: Quartz Arenite


Age period: Carboniferous/Permian

Name: Fossiliferous Limestone


Age period: Devonian/ordovician

Name: Fossiliferous Shale


Age period: Cambrian

Name: Conglomerate



Name: Gneiss


Age period: Neoarchean Eon

Name: Welded Tuff


Age period: Jurassic Period

Name: Syenite



Name: Serpentined Dunite


Description: Waxy lustre, lack of texture = alteration of half minerals, serpentine, pyroxene


Position: Upper mantle Periodtites

Name: Gabbro


Position: Upper magma chamber


Description: mafic, phaneritic, serpentine, course grained, pyroxene, plagioclase, feldspar, intrusive - slow cooling

Name: Serpentined Dunite


Position: Lower magma chamber


Description: serpentine, chromite, phaneritic, mafic, chromite sinks, serpentine rises

Name: Diabase


Position: Sheeted dykes


Description: porphyritic

Name: Amygdaloidal Basalt


Position: pillow lavas


Description: vesicles, high volatile content, aphanetic

Name: Mudstone


Position: sediment cover


Description: non-fissile, massive, low energy environment, soft sediment deformation = uneven surface

Name: Amphibolitized Perioditite


position: Upper mantle periodotite


Description: cooled slowly at depth

Name: Chert


Position: sediment cover


Description: precipitation of silica gel or deposition of silicious ooze, chert identified by hardness and fine grained soft sediment deformation present, biochemical

Name: Conglomerate


Position: Frontal arc/mountain lowlands


Why? Repeated rounding and sorting of class by long stream transportation. Physical weathering produces rock fragments which are transported down hill by gravity, with assistance from water.

Name: Quartz Arenite


Position: forearc basin


Why? Travels a far distance (fine grained) compared to breccia and conglomerate

Name: Amphibolite


Postion: Volcanic arc


Why? relatively uniform pressure and heat, but higher pressure and heat than green schist, found under the volcanic arc. Regional metamorphic facies.

Name: Ignimbrite


Postion: Volcanic arc


Why? formed from pyroclastic flow that remelted and weld. Lava flows and true ignimbrite are found close to the original volcano

Name: Shale


Position: forearm basin


Why? Sediments carried offshore become concentrated here. Land derived character of the sediment is evident in the nature of fossil components preserved in the shale - light weight plant debris swept out to sea by floods.

Name: Turbidites


Position: Trench


Why? Deposited by turbidity currents. high sediment production here from the rapid erosion of high lands. narrow widths of continental shelf areas landward and steep stop of seafloor leading to trench

Name: Chlorite Schist


Position: forearc basin


why? foliated and chlorite = chlorite schist at green schist facies

Name: Eclogite


Position: Deep subduction zone


Why? high temperature and pressure is found in the deep subduction zone

Name: Breccia/Conglomerate


Position: Frontal arc/mountain lowland


Why? collision = upthrust of rock = numerous high mountains. Physical weathering = rock fragments. Transported downstream by gravity and water.

Name: Conglomerate



Name: Shale


Position: river channel and floodplain


Why? footprint = periods of exposure. Ripple cross bedding form when flood water escape a river channel and velocity decreases so fine sediment settles out to from thin layers.

Name: Quartz Arenite


Position: Beaches, barrier island dunes.


Why? well sorted quartz sandstone and well rounded grains imply repeated processing of the same sediment grains by waves again and again

Name: Granular Sandstone (3-7b)


Position: Alluvial fan


why? Variable composition --> close to source, K-feldspar --> arid conditions

Name: Oolitic Limestone


Position: beaches, barriers islands, dunes


Why? ooids tend to from well sorted deposits of oolitic limestone in agitated tropical beach or shallow nearshore marine shelf environment

Name: Stromatolitic limestone


Position: tidal flats


Why? highly saline conditions that develop on mud flats in air tropical regions can promote the development of stromatolites

Name: Carbonaceous Shale


Positions: Deltas


Why? Mud = calm water, Plant fossils = close to land

Name: Diamictite


Position: upland and glacial environments


Why? sediment is very poorly sorted and is massive with very large clasts floating in a mud matrix. Scratches on large clasts imply a glacial origin.

Name: Microbial mats - limestone


Position: Lagoon


Why? biochemical so it needs to have a low energy quiet shallow body of water where it experiences high rates of evaporation and dries out, producing hyper saline and oxygen-deficient conditions

Name: Shale


Position: deep marine environment


Why? fine grained = calm water, shells deposited during storms, impression of marine life

Name: Shale


Position: deep sea floor


Why? impression of marine life, fine grained = calm water

Name: Quartz Arenite


Position: tidal flats


Why? mud cracks indicate alternating wet and dry periods in a low energy environment, well sorted sandstones = far from source

Name: Scoria

Name: Obsidian

Name: Pumice

Name: Lapilli Tuff

Name: Porphyry

Name: Quartz Diorite

Name: Granite

Name: Pegmatite

Names: (From right to left): I-1137/15, I-9d, DT, I-122

Name: I-3

Name: I-15

Name: Quartz Arenite

Name: Shale

Name: Claystone

Name: Greywake

Name: Quartz Arenite

Name: Conglomerate

Name: Breccia

Name: Conglomerate

Name: Chert

Name: BIF

Name: Chert

Name: Coal

Name: Fossiliferous Limestone

Name: Quartz Arenite

Name: Lithos Arenite

Name: Stromatolitic Limestone

Name: Mudstone