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Mudstone, a type of mudrock, is a fine-grained sedimentary rock whose original constituents were clays or muds. Grain size is up to 0.063 millimetres (0.0025 in) with individual grains too small to be distinguished without a microscope. With increased pressure over time, the platy clay minerals may become aligned, with the appearance of fissility or parallel layering.
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microscopes called "polarizing" or "pol" for short. After development in the late 19th century, pol scopes became critical tools for studying the minerals and structures of rocks (our Earth), which can tell us much about how they formed. The objective of this chapter is to evaluate some of the proposed classifications
of sedimentary carbonate rocks, and to present suggestions for naming and describing them.
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