Abstract
Claystones immediately overlying the early Eocene age ocean-floor basalt underwent hydrothermal and thermal alterations originating from the basalt, which resulted in changes in both the mineralogical and chemical composition of the sediments. -from Authors
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CITATION STYLE
APA
Nielsen, O. B., Cremer, M., Stein, R., Thiebault, F., & Zimmerman, H. (1989). Analysis of sedimentary facies, clay mineralogy, and geochemistry of the Paleogene sediments of Site 647, Labrador Sea. Proc., Scientific Results, ODP, Leg 105, Baffin Bay and Labrador Sea, 101–110. https://doi.org/10.2973/odp.proc.sr.105.116.1989
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