Exam 6: Sedimentary Rocks the Archives of Earth History

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The three major depositional environments are ____________________, ____________________, and ____________________.

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continental, transitional, marine,
continental, marine, transitional,
transitional, continental, marine,
transitional, marine, continental,
marine, continental, transitional,
marine, transitional, continental

Compare and contrast the various types of depositional environments in which evaporite deposits form. How do these deposits differ?

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Evaporite deposits may be formed in playa lakes and saline lakes in desert areas. However, these deposits generally are relatively thin and small in areal extent. In contrast, silled (barred) marine basins (see Fig. 3 in the Perspectives section of Chapter 6) commonly are the site of deposition of thick evaporite deposits of salt and gypsum. In some cases, evaporation of large seas that are closed to other oceans and seas may be responsible for thick marine evaporite deposits.

Lagoons and reefs are sites of carbonate deposition.

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The chemical formula for dolomite is CaCO3.

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In a well-sorted rock, ____.

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Because wind has a limited capacity to transport sediment, wind deposits are poorly sorted.

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Explain how fossils, and especially microfossils, can be used to help determine ancient depositional environments.

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The most common chemical sedimentary rock is ____.

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In bioturbation, most of the original sedimentary structures are preserved.

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The most important source rocks for fuels we use today are igneous rocks.

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Graded bedding forms when ____.

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Compare and contrast the sediments deposited in continental, transitional, and marine environments. Give specific examples of these sediment types and the environments where they commonly form.

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From continent to deep-ocean basin, what is the order of offshore environments?

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Turbidity currents deposit sediments in ____ beds with ____.

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Prograding d elta deposits differ from turbidity current deposits because ____.

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Rocks above and below a bedding plane may have different physical properties.

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A well-sorted sediment contains particles that are of about the same size.

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Cross-bedding can form via wind or water currents.

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Graded beds refer to sedimentary beds that show a decrease in grain size from bottom to top.

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____ are transitional environments because they ____.

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