(Table 1) Heat flow in the Red Sea rift zone at 18°N
View DatasetVerzhbitsky, Evgeny V;Zolotarev, Vladimir G
Description
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.
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Publication Details
Subfield
Materials Chemistry
Field
Materials Science
Domain
Physical Sciences
Confidence Score
48%
Source
Scholar Data Model
Keywords
Event labelLatitude of eventLongitude of eventElevation of eventTemperature (thermal) gradientConductivity, thermalHeat flowGravity corerThermistorCalculatedPIKARArchive of Ocean Data (ARCOD)