Basal dolomitic sediments, Tyrrhenian Sea, Ocean Drilling Program Leg 107

J. A. McKenzie; A. Isern; A. M. Karpoff; P. K. Swart

doi:10.2973/odp.proc.sr.107.124.1990

Basal dolomitic sediments, Tyrrhenian Sea, Ocean Drilling Program Leg 107

J. A. McKenzie, A. Isern, A. M. Karpoff, P. K. Swart

Research output: Contribution to journal › Article › peer-review

5 Scopus citations

Abstract

These sediments overlie the basaltic basement complex and are enriched in iron, and in some instances, also in manganese. The manganese enrichments, together with a very slight enrichment in trace transition elements, strongly suggest that the basal sediments have an affinity to deep-sea metalliferous deposits of hydrothermal origin. -from Authors

Original language	English (US)
Pages (from-to)	141-152
Number of pages	12
Journal	Unknown Journal
DOIs	https://doi.org/10.2973/odp.proc.sr.107.124.1990
State	Published - 1990
Externally published	Yes

ASJC Scopus subject areas

Environmental Science(all)
Earth and Planetary Sciences(all)

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10.2973/odp.proc.sr.107.124.1990

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title = "Basal dolomitic sediments, Tyrrhenian Sea, Ocean Drilling Program Leg 107",

abstract = "These sediments overlie the basaltic basement complex and are enriched in iron, and in some instances, also in manganese. The manganese enrichments, together with a very slight enrichment in trace transition elements, strongly suggest that the basal sediments have an affinity to deep-sea metalliferous deposits of hydrothermal origin. -from Authors",

author = "McKenzie, {J. A.} and A. Isern and Karpoff, {A. M.} and Swart, {P. K.}",

year = "1990",

doi = "10.2973/odp.proc.sr.107.124.1990",

language = "English (US)",

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journal = "Scientific Computing and Instrumentation",

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publisher = "Springer Wien",

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AU - Karpoff, A. M.

AU - Swart, P. K.

PY - 1990

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AB - These sediments overlie the basaltic basement complex and are enriched in iron, and in some instances, also in manganese. The manganese enrichments, together with a very slight enrichment in trace transition elements, strongly suggest that the basal sediments have an affinity to deep-sea metalliferous deposits of hydrothermal origin. -from Authors

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