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1 Metamorphic Rocks Metamorphic Rocks Metamorphism – The transformation of pre-existing rocks into new types by the action of heat and pressure changes. Photos by C.C. Plummer

Metamorphic Rocks rocks.pdf · types by the action of heat and pressure changes. Heat – from magma intrusion, compression, or decay of radioactive elements. Generally, at depths

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Page 1: Metamorphic Rocks rocks.pdf · types by the action of heat and pressure changes. Heat – from magma intrusion, compression, or decay of radioactive elements. Generally, at depths

1

Metamorphic Rocks

Metamorphic Rocks

Metamorphism – The transformation of pre-existing rocks into new types by the action of heat and pressure changes.

Photos by C.C. Plummer

Page 2: Metamorphic Rocks rocks.pdf · types by the action of heat and pressure changes. Heat – from magma intrusion, compression, or decay of radioactive elements. Generally, at depths

2

Metamorphic Rocks

Metamorphism – The transformation of pre-existing rocks into new types by the action of heat and pressure changes.

Heat – from magma intrusion, compression, or decay of radioactive elements. Generally, at depths of about 35 km, temps are high enough to begin melting rocks.

Metamorphic Rocks

Metamorphism – The transformation of pre-existing rocks into new types by the action of heat and pressure changes.

Pressure – generates heat, and along points of contact can melt rocks. Also generates the development of banded and foliated textures. Increasing pr4essure conditions force grains closer together and eliminates pore space.

Page 3: Metamorphic Rocks rocks.pdf · types by the action of heat and pressure changes. Heat – from magma intrusion, compression, or decay of radioactive elements. Generally, at depths

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Metamorphic Rocks

Metamorphism – The transformation of pre-existing rocks into new types by the action of heat and pressure changes.

Chemically active fluids – chemical exchange of elements generate different mineral compositions.

Metamorphic Rocks

Two different types of metamorphism:

1. Contact metamorphism –occurs upon contact of hot igneous rocks and surrounding country rocks. As distance from intrusion increases degree of metamorphism decreases.

Page 4: Metamorphic Rocks rocks.pdf · types by the action of heat and pressure changes. Heat – from magma intrusion, compression, or decay of radioactive elements. Generally, at depths

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Metamorphic Rocks

Two different types of metamorphism:

1. Regional metamorphism –occurs upon contact of hot igneous rocks and surrounding country rocks. As distance from intrusion increases degree of metamorphism decreases.

Metamorphic Rocks

Identifying metamorphic rocks using texture.

Foliation – parallel arrangement of minerals

Photos by C.C. Plummer

Page 5: Metamorphic Rocks rocks.pdf · types by the action of heat and pressure changes. Heat – from magma intrusion, compression, or decay of radioactive elements. Generally, at depths

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Metamorphic Rocks

Identifying metamorphic rocks using texture.

Foliated rocks:

Slate – metamorphosed clayey rocks (shale). Sheety appearance

Photo by C.C. Plummer Photo by P.D. Rowley, USGS

Metamorphic Rocks

Identifying metamorphic rocks using texture.

Foliated rocks:

Schist

Photo by C.C. Plummer

Page 6: Metamorphic Rocks rocks.pdf · types by the action of heat and pressure changes. Heat – from magma intrusion, compression, or decay of radioactive elements. Generally, at depths

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Metamorphic Rocks

Identifying metamorphic rocks using texture.

Foliated rocks:

Gneiss

Metamorphic Rocks

Identifying metamorphic rocks using texture.

Foliated rocks:

Gneiss

Photo by C.C. Plummer

Page 7: Metamorphic Rocks rocks.pdf · types by the action of heat and pressure changes. Heat – from magma intrusion, compression, or decay of radioactive elements. Generally, at depths

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Metamorphic Rocks

Identifying metamorphic rocks using texture.

Nonfoliated rocks:

Marble

Quartzite

Photo by C.C. Plummer