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Non-Terrigenous Sediments and Rocks

Non-Terrigenous Sediments and Rocks. Carbonate Sediments and Rocks. Most form as biogenic particles (essentially the only source) in warm (tropical; 30 o N to 30 o S latitude), shallow (shelf; within the photic zone), (mostly <10-20 m) marine water Also accumulate in deepwater ooze

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Mainly diagenetic - PowerPoint PPT Presentation

Non-Terrigenous Sediments and Rocks