Composition of barite crusts and basalts from the Red Sea rift zone

Barite ores with admixture of sphalerite that occur in the Atlantis-II Deep are indicated by their geological position, structure, and mineral and chemical characteristics and by isotope composition of sulfur and oxygen in them to be of hydrothermal origin. They were produced close to an orifice of an intermittent hydrothermal vent by chemogenic precipitation of barite onto cooled basalt.

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Cite this as

Sval'nov, Vyacheslav N, Strizhov, Valentin P, Bogdanov, Yury A, Isaeva, Alexandra B (1984). Dataset: Composition of barite crusts and basalts from the Red Sea rift zone. https://doi.org/10.1594/PANGAEA.756430

DOI retrieved: 1984

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.756430
Author Sval'nov, Vyacheslav N
Given Name Vyacheslav N
Family Name Sval'nov
More Authors
Strizhov, Valentin P
Bogdanov, Yury A
Isaeva, Alexandra B
Source Creation 1984
Publication Year 1984
Resource Type application/zip - filename: Svalnov_1984
Subject Areas
Name: Oceans

Related Identifiers
Title: Hydrothermal barite crust on basalts in the Atlantis-II Deep (Red Sea)
Type: DOI
Relation: IsSupplementTo
Year: 1984
Source: Oceanology
Authors: Sval'nov Vyacheslav N , Strizhov Valentin P , Bogdanov Yury A , Isaeva Alexandra B .