Metamorphic Rocks Flashcards
Texture
sizes, shapes, and arrangements
Foliated metamorphic rocks
layering and parallel alignment of platy (flat) mineral crystals
E.g. micas
How does foliated rock occur
result of pressure (shearing and smearing of crystals) and recrystallization
Slaty rock cleavage
very flat foliation
developed along flat, parallel, closely spaced shear planes in tightly folded clay or mica rich rocs
Slate
rocks with excellent slaty cleaving
Phyllite Texture
wavy and/or wrinkled foliation or fine grained platy minerals
intermediate grade metamorphism
metallic luster
developed oblique or perpendicular to weak slaty cleavage
Phylite
fine grained metamorphic rock
satiny, silver, green, brassy, metallic cluster
wavy foliation
wrinkled appearance
Schistosity
scaly glittery layering of visible (medium-course grained) platy materials and/or linear alignment of long prismatic crystals
intermediate - high metamorphism
Schist
medium-course grained, scaly, foliated metamorphic rock
formed by intermediate-grade-metamorphism mud,shale, slate, other rocks rich in clay
Gneissic Banding
alternating layers or lenses of light and dark medium - course grained minerals
high grade metamorphism
Non foliated metamorphic rocks
no obvious layering (foliates)
stretched fossils, long prismatic crystals grown parallel to the pressure field
Crystalline Texture
medium-coarse grained aggregate of inter grown, equal sized, visible crystals
non foliated
Gneiss
medium-course grained rock
biotite/quartz
Marble
fine-course grained
non foliated
intermediate- high grade metamorphism
Microcrystalline Texture
fine grained aggregate of inter grown microscopic crystals
non foliated