Relation between Chemical Composition and Sedimentation Rate of Pacific Ocean-Floor Sediments Deposited since the Middle Cretaceous: Basic Evidence for Chemical Constraints on Depositional Environments of Ancient Sediments
Chemical characteristics of Pacific marine sediments were examined for different environments operating since the middle Cretaceous. As a result of the examinations, a procedure for evaluating depositional environments of ancient sediments in orogenic belts is proposed. The concentration of hydrogen...
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Veröffentlicht in: | The Journal of geology 1984-05, Vol.92 (3), p.235-259 |
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Sprache: | eng |
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