Heat flow in the Black and Mediterranean seas

Results of heat-flow measurements in the western Black Sea and within the African-Sicilian region of the Mediterranean Sea are presented. New data reveal a well-defined correlation with the deep-seated geologic structure of the regions examined. A heat-flow anomaly within the Pantelleria graben, in the authors' opinion, is a consequence of connective heat transfer along channels of disjunctive faults.

Data and Resources

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Cite this as

Zolotarev, Vladimir G, Sochel'nikov, V V, Malovitskiy, Ya P (1979). Dataset: Heat flow in the Black and Mediterranean seas. https://doi.org/10.1594/PANGAEA.755378

DOI retrieved: 1979

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.755378
Author Zolotarev, Vladimir G
Given Name Vladimir G
Family Name Zolotarev
More Authors
Sochel'nikov, V V
Malovitskiy, Ya P
Source Creation 1979
Publication Year 1979
Resource Type application/zip - filename: Zolotarev_1979
Subject Areas
Name: Oceans

Related Identifiers
Title: Results of heat-flow measurements in the Black and Mediterranean Sea basins
Type: DOI
Relation: IsSupplementTo
Year: 1979
Source: Oceanology
Authors: Zolotarev Vladimir G , Sochel'nikov V V , Malovitskiy Ya P .