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

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Verzhbitsky, 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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Mentions (0)

Metrics

Dataset Index

0.8

FAIR Score

96%

Citations

0

Mentions

0

Metrics Over Time

Publication Details

DOI

Publisher

PANGAEA

Assigned Domain

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)

Normalization Factors

FT

42.31

CTw

1.00

MTw

1.00