(Table 1) Heat flow in the Red Sea rift zone at 18°N

DOI

New results of geothermal studies at 18°N in the Red Sea rift zone are discussed. It was established that the thermal field of the African plate in this area has a higher than ordinary level, and averages 3.0-3.5 UTF. Heat flow of the Arabian plate is characterized by negative anomalies and is local in character in comparison to adjoining areas of the rift.

Supplement to: Verzhbitsky, Evgeny V; Zolotarev, Vladimir G (1980): Studies of the heat flow in the rift zone of the Red Sea. Oceanology, 20(5), 580-583

Identifier
DOI https://doi.org/10.1594/PANGAEA.755166
Metadata Access https://ws.pangaea.de/oai/provider?verb=GetRecord&metadataPrefix=datacite4&identifier=oai:pangaea.de:doi:10.1594/PANGAEA.755166
Provenance
Creator Verzhbitsky, Evgeny V; Zolotarev, Vladimir G
Publisher PANGAEA
Publication Year 1980
Rights Creative Commons Attribution 3.0 Unported; https://creativecommons.org/licenses/by/3.0/
OpenAccess true
Representation
Resource Type Supplementary Dataset; Dataset
Format text/tab-separated-values
Size 45 data points
Discipline Earth System Research
Spatial Coverage (39.785W, 17.888S, 40.245E, 18.235N); Red Sea