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Verzhbitsky, Evgeny V; Zolotarev, Vladimir G (1980): (Table 1) Heat flow in the Red Sea rift zone at 18°N [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.755166, Supplement to: Verzhbitsky, EV; Zolotarev, VG (1980): Studies of the heat flow in the rift zone of the Red Sea. Oceanology, 20(5), 580-583

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Abstract:
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.
Project(s):
Coverage:
Median Latitude: 18.055211 * Median Longitude: 40.045030 * South-bound Latitude: 17.888300 * West-bound Longitude: 39.785000 * North-bound Latitude: 18.235000 * East-bound Longitude: 40.245000
Minimum Elevation: -1410.0 m * Maximum Elevation: -686.0 m
Event(s):
PS-226 * Latitude: 17.888300 * Longitude: 39.813300 * Elevation: -686.0 m * Location: Red Sea * Campaign: PIKAR * Method/Device: Gravity corer (GC)
PS-228 * Latitude: 17.938300 * Longitude: 39.955000 * Elevation: -1210.0 m * Location: Red Sea * Campaign: PIKAR * Method/Device: Gravity corer (GC)
PS-289 * Latitude: 18.168333 * Longitude: 40.176667 * Elevation: -1410.0 m * Location: Red Sea * Campaign: PIKAR * Method/Device: Gravity corer (GC)
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1Event labelEvent
2Latitude of eventLatitude
3Longitude of eventLongitude
4Elevation of eventElevationm
5Temperature (thermal) gradientT grad10-3 °C/cmVerzhbitsky, Evgeny V
6Conductivity, thermalkW/m/KVerzhbitsky, Evgeny V
7Heat flowHFmW/m2Verzhbitsky, Evgeny VThermistorobserved
8Heat flowHFmW/m2Verzhbitsky, Evgeny VCalculatedcorrected for sedimentation and contrast between thermal conductivity and thermal diffusivity
9Heat flowHFmW/m2Verzhbitsky, Evgeny VCalculatedequilibrium with correction for relief
Size:
45 data points

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