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):
Archive of Ocean Data (ARCOD)
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):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | Event label | Event | ||||
2 | Latitude of event | Latitude | ||||
3 | Longitude of event | Longitude | ||||
4 | Elevation of event | Elevation | m | |||
5 | Temperature (thermal) gradient | T grad | 10-3 °C/cm | Verzhbitsky, Evgeny V | ||
6 | Conductivity, thermal | k | W/m/K | Verzhbitsky, Evgeny V | ||
7 | Heat flow | HF | mW/m2 | Verzhbitsky, Evgeny V | Thermistor | observed |
8 | Heat flow | HF | mW/m2 | Verzhbitsky, Evgeny V | Calculated | corrected for sedimentation and contrast between thermal conductivity and thermal diffusivity |
9 | Heat flow | HF | mW/m2 | Verzhbitsky, Evgeny V | Calculated | equilibrium with correction for relief |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
45 data points
Data
1 Event | 2 Latitude | 3 Longitude | 4 Elevation [m] | 5 T grad [10-3 °C/cm] | 6 k [W/m/K] | 7 HF [mW/m2] (observed, Thermistor) | 8 HF [mW/m2] (corrected for sedimentation a...) | 9 HF [mW/m2] (equilibrium with correction f...) |
---|---|---|---|---|---|---|---|---|
PS-226 | 17.8883 | 39.8133 | -686 | 2.10 | 0.83 | 175 | 194 | 200 |
PS-228 | 17.9383 | 39.9550 | -1210 | 2.50 | 0.83 | 208 | 231 | 231 |
PS-289 | 18.1683 | 40.1767 | -1410 | 0.38 | 0.72 | 27 | 30 | 29 |
PS-290 | 18.1853 | 40.1853 | -1100 | 0.40 | 0.71 | 28 | 32 | 33 |
PS-301 | 17.9467 | 39.8900 | -1157 | 0.46 | 0.84 | 38 | 43 | 41 |
PS-311 | 18.0600 | 40.1800 | -1350 | 0.45 | 0.76 | 34 | 38 | 38 |
PS-358 | 18.2350 | 39.7850 | -1360 | 1.40 | 0.83 | 117 | 130 | 130 |
PS-369a | 18.0750 | 40.1750 | -1370 | 0.35 | 0.82 | 28 | 32 | 32 |
PS-369b | 18.0000 | 40.2450 | -1360 | 0.50 | 0.78 | 39 | 43 | 43 |