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- W2279454075 abstract "About 10.8 million tons pr year of detrital carbonate material is brought into the Black Sea in suspension by rivers; more than 25 million tons is carried in solution. In addition, authigenic carbonates, principally mollusk shell and coccoliths, are formed within the Black Sea. The grain-size of carbonate sediments varies as a function of composition and origin. Carbonate material consists mainly of low-magnesium calcite and aragonite. It is concluded that biogenic processes are the major factor in modern carbonate sedimentation. Yet terrigenous carbonate material also is significant in the general process of carbonate sedimentation." @default.
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- W2279454075 title "Some Characteristics of Carbonate Sedimentation in Black Sea: Sediments" @default.
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