Residual Sediments of the Vema Fracture Zone, Central Atlantic
Residual Sediments of the Vema Fracture Zone, Central Atlantic
About this item
Full title
Author / Creator
Publisher
Moscow: Pleiades Publishing
Journal title
Language
English
Formats
Publication information
Publisher
Moscow: Pleiades Publishing
Subjects
More information
Scope and Contents
Contents
The Vema Fracture Zone orthogonally intersecting the Mid-Atlantic Ridge along 11° N is a complex tectono-sedimentary system, through which bottom water is transferred from the western to the eastern Atlantic. The southern surrounding of the fault valley is an extended (about 320 km) transverse ridge. At the early stages of the Vema System evolution...
Alternative Titles
Full title
Residual Sediments of the Vema Fracture Zone, Central Atlantic
Authors, Artists and Contributors
Author / Creator
Identifiers
Primary Identifiers
Record Identifier
TN_cdi_proquest_journals_2441293240
Permalink
https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_proquest_journals_2441293240
Other Identifiers
ISSN
0024-4902
E-ISSN
1608-3229,1573-8892
DOI
10.1134/S0024490220050028
