Inorganic major, minor and trace element geochemistry and clay mineralogy of sediments from the Deep Sea Drilling Project Leg 96, Gulf of Mexico.

K. T. Pickering; D. A.V. Stow

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Inorganic major, minor and trace element geochemistry and clay mineralogy of sediments from the Deep Sea Drilling Project Leg 96, Gulf of Mexico.

Initial reports DSDP, Leg 96, Ft. Lauderdale to Galveston, Texas, 1983 (1986) 733-745

DOI: 10.2973/dsdp.proc.96.144.1986

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Abstract

Clay mineral composition at all the sites is smectite:illite:chlorite:kaolinite in the approximate percentage ratio 50:20:20:10. Geochemical results indicate only slight variation between and within the sites. Variation in the major, minor, and trace element composition can be explained by a change in the relative abundance of quartz, clay minerals, and carbonates. -from Authors

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Pickering, K. T., & Stow, D. A. V. (1986). Inorganic major, minor and trace element geochemistry and clay mineralogy of sediments from the Deep Sea Drilling Project Leg 96, Gulf of Mexico. Initial Reports DSDP, Leg 96, Ft. Lauderdale to Galveston, Texas, 1983, 733–745. https://doi.org/10.2973/dsdp.proc.96.144.1986

Inorganic major, minor and trace element geochemistry and clay mineralogy of sediments from the Deep Sea Drilling Project Leg 96, Gulf of Mexico.

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