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Metamorphic Rocks and Conclusion of Sedimentary Rocks

Metamorphic Rocks and Conclusion of Sedimentary Rocks

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Page 1: Metamorphic Rocks and Conclusion of Sedimentary Rocks

Metamorphic Rocks and Conclusion of Sedimentary

Rocks

Page 2: Metamorphic Rocks and Conclusion of Sedimentary Rocks

The deal with sedimentary rocks

• The bigger the grains, the higher the energy of the depositional environment in which it was formed.

• The smaller the grains, the quieter the environment in the rock formed.

• SEDIMENTARY ROCKS ARE SO USEFUL BECAUSE THEY RECORD THE EARTH’S HISTORY. THEY TELL US WHAT KIND OF ENVIRONMENT WAS WHERE AND WHEN.

Page 3: Metamorphic Rocks and Conclusion of Sedimentary Rocks

Stratification

• Since sedimentary rocks are formed by deposition of sediment, they form layers of rock.

• Stratification occurs when you get distinct layering in rocks (you deposit something different on top of something else).

• Principle of Uniformitarianism and Suposition – each layer is uniform in composition, older layers are on bottom, newer layers on top.

• If there is discontinuity in the layers, geologists term it an unconformity.

Page 4: Metamorphic Rocks and Conclusion of Sedimentary Rocks

How can you get an unconformity?

• Erosion of a layer just deposited.

• Faulting (normal or reverse)

• For reverse faulting, your older rocks would get pushed on top and mess up the order.

Page 5: Metamorphic Rocks and Conclusion of Sedimentary Rocks

Cool Sed rock features

• Cross-bedding – formed from changes in wind direction, or change in direction of water current.

• Ripple marks – you can definitely tell which way water or wind moved

• Mudcracks – formed when mud dries up and shrinks

• Geodes- water within sediments leaches into cavities of rocks precipitating calcite or quartz crystals

Page 6: Metamorphic Rocks and Conclusion of Sedimentary Rocks

Metamorphic Rocks

• Metamorphism (in the geological sense)- the changing of one rock into another by inducing heat and/or pressure.

• Two types of metamorphism: contact, and regional

Page 7: Metamorphic Rocks and Conclusion of Sedimentary Rocks

Contact Metamorphism

• When rocks are changed by heat

• How this happens:

1.) rocks that are subducted and come in contact with magma

2.) rocks happen to come into contact with magma that is migrating towards the surface (some new volcanism)

Page 8: Metamorphic Rocks and Conclusion of Sedimentary Rocks

Regional Metamorphism

• Rock change because they undergo some kind of process that induces a lot of pressure

• How this happens:

1.) rock in a subduction zone, the deeper you go, the more pressure you encounter

2.) rock in a fault zone (lots of pressure there)

3.) compressional forces via plate tectonics, isostatic adjustment, remember folding?????? Ductile deformation?

Page 9: Metamorphic Rocks and Conclusion of Sedimentary Rocks

Chemical Alteration

• Hydrothermal – pretty much water eruptions- water comes into contact with magma, the magma boils it an sends it back to the surface enriched with chemicals from the subsurface and magma chamber

Page 10: Metamorphic Rocks and Conclusion of Sedimentary Rocks

How you can tell if a rock is formed by contact or regional

metamorphism.• One word: FOLIATION• Foliated rocks have visible parallel banding. A lot

of the time these bands are wavy, warped, because after all, they were formed under pressure. So, FOLIATED ROCKS ARE FORMED BY REGIONAL METAMORPHISM.

• Non-foliated – most of the time are rocks formed by contact metamorphism

• An example: marble – it’s a non foliated rock formed by regional metamorphism