Patterns in the Redistribution of Substances During Diagenesis of Sediments in Humid Zones: The Carbonate Concretions
The redistribution of substances is one of the characteristic features of diagenesis; and it has not been given adequate attention until now. Here, however, we confine ourselves to a mere statement of the facts of redistribution and make no attempt to delve deeply into a study of the problem.
KeywordsFacies Type Coal Measure Humid Zone Authigenic Mineral Carbonate Concretion
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