Metamorphic Rocks (Transitional/Non-foliated to foliated textures) Flashcards
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.
Metaconglomerate
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.
Serpentinite
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.
Soapstone
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.
Greenstone
Sodium-rich basalt that can occur in greenstones.
Spilite
Sodium-rich andesite that can occur in greenstones.
Keratophyte
A greenstone characterized by the abundance of chlorite, epidote, prehnite, pumpellyite, talc, serpentine, actinolite and albite, with a foliated texture.
Greenschist
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
Amphibolite
Amphibolites derived from basic igneous rocks.
Ortho-amphibolite
Amphibolites derived from sedimentary protoliths.
Para-amphibolite
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.
Granulite
Schistose metamorphic rocks produced in subduction zone settings, characterized by significant amount of glaucophane, lawsonite, aegirine and kyanite.
-also characterized by its blue color
Blueschist
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.
Eclogite