Metamorphic Rocks (Transitional/Non-foliated to foliated textures) Flashcards

1
Q

Metamorphic rocks derived from conglomerate protoliths and contain sub-rounded to rounded relict clasts with >2 mm diameter, and can form from a wide range of protolith clast compositions from burial, dynamothermal or contact metamorphism.

A

Metaconglomerate

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2
Q

Serpentine-rich metamorphic rocks that can occur either foliated or non-foliated forms that form form through hydrothermal alteration of ultrabasic rocks at temperatures below-500 °C, hydrating olivines and pyroxenes into serpentine minerals.

A

Serpentinite

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3
Q

Fine-grained alteration rocks produced from the alteration of ultrabasic rocks or Mg-rich sedimentary rocks through low temperature and pressure hydrothermal fluids, where Talc contributes to its soapy feel and low hardness.

A

Soapstone

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4
Q

Green-colored metamorphic rocks rich in silicate minerals that commonly include chlorite, epidote, prehnite, pumpellyite, talc, serpentine, actinolite, albite, forms by low to moderate (200-500 °C) temperature alteration of basic to ultrabasic igneous rocks, and commonly develop from hydrothermal metamorphism in oceanic crust near divergent plate boundaries.

A

Greenstone

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5
Q

Sodium-rich basalt that can occur in greenstones.

A

Spilite

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6
Q

Sodium-rich andesite that can occur in greenstones.

A

Keratophyte

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7
Q

A greenstone characterized by the abundance of chlorite, epidote, prehnite, pumpellyite, talc, serpentine, actinolite and albite, with a foliated texture.

A

Greenschist

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8
Q

Dark-colored metamorphic rocks composed largely of amphiboles, and form by medium to high temperature (>550 °C) regional metamorphism of basic igneous rocks or sedimentary rocks

A

Amphibolite

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9
Q

Amphibolites derived from basic igneous rocks.

A

Ortho-amphibolite

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10
Q

Amphibolites derived from sedimentary protoliths.

A

Para-amphibolite

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11
Q

Medium- to coarse-grained rocks that contain granoblastic to foliated textures that form by high temperature (>800 °C) and high pressure (>10 kbar, or -33 km depth) metamorphism.

A

Granulite

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12
Q

Schistose metamorphic rocks produced in subduction zone settings, characterized by significant amount of glaucophane, lawsonite, aegirine and kyanite.
-also characterized by its blue color

A

Blueschist

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13
Q

Very high pressure, high
temperature rocks that develop principally from basic protoliths, and may be the major rock type in Earth’s lower crust due to its high temperature (>400 °C) and high pressure (1.2 GPa at >40 km depth) conditions. It commonly appears as red and green due to its major minerals being jadeite, pyroxene, omphacite, and red garnets.

A

Eclogite

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