(Table 1) Heat flow in the Red Sea rift zone at 18°N
| Cobertura |
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 |
|---|---|
| Data(s) |
13/12/1980
|
| Resumo |
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. |
| Formato |
text/tab-separated-values, 45 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.755166 doi:10.1594/PANGAEA.755166 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Fonte |
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 |
| Palavras-Chave | #Archive of Ocean Data; ARCOD; Calculated; Conductivity, thermal; Elevation of event; Event label; GC; Gravity corer; Heat Flow; Latitude of event; Longitude of event; PIKAR; PS-226; PS-228; PS-289; PS-290; PS-301; PS-311; PS-358; PS-369a; PS-369b; Red Sea; Temperature (thermal) gradient; Thermistor |
| Tipo |
Dataset |
