Composition of bottom sediments and serpentinites from Core PS-846

A core of foraminiferal-coccolithic oozes filling a valley of the transform fault located at 29°40'S on the South Atlantic Ridge contains layers composed of angular fragments of igneous and metamorphic rocks. They include many serpentinites deriving from serpentinized ultrabasic rocks, probably exposed on the lower section of the southern slope of the fault valley. A mineral and chemical description of these serpentinites is given.

Data and Resources

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Cite this as

Trimonis, Egidius S, Emelyanov, Emelyan M, Kharin, Gennady S (1987). Dataset: Composition of bottom sediments and serpentinites from Core PS-846. https://doi.org/10.1594/PANGAEA.756596

DOI retrieved: 1987

Additional Info

Field Value
Imported on November 30, 2024
Last update November 30, 2024
License CC-BY-3.0
Source https://doi.org/10.1594/PANGAEA.756596
Author Trimonis, Egidius S
Given Name Egidius S
Family Name Trimonis
More Authors
Emelyanov, Emelyan M
Kharin, Gennady S
Source Creation 1987
Publication Year 1987
Resource Type application/zip - filename: Trimonis_1987
Subject Areas
Name: Oceans

Related Identifiers
Title: Serpentinites in sediments from the zone of a transform fault on the South Atlantic Ridge
Type: DOI
Relation: IsSupplementTo
Year: 1987
Source: Oceanology
Authors: Trimonis Egidius S , Emelyanov Emelyan M , Kharin Gennady S .