Kondyurin, A V; Sochel'nikov, V V (1983): (Table 1) Heat flow data in the western Black Sea. PANGAEA, https://doi.org/10.1594/PANGAEA.755928, Supplement to: Kondyurin, AV; Sochel'nikov, VV (1983): Geothermal flow in the western part of the Black Sea. Oceanology, 23(4), 468-472
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Results of heat flow measurements are presented. On the basis of new data on structure of the sedimentary sequence, corrections are introduced that take account of effect of sedimentation. Diagrammatic maps of distribution of observed and deep-seated heat flow have been constructed. A hypothesis is offered that the regional zone of anomalously high heat-flow values on the northern continental slope has been controlled by processes of subsidence of an oceanic plate beneath its continental counterpart.
Median Latitude: 42.694872 * Median Longitude: 31.117949 * South-bound Latitude: 41.616667 * West-bound Longitude: 29.416667 * North-bound Latitude: 44.166667 * East-bound Longitude: 33.333333
Minimum Elevation: -2225.0 m * Maximum Elevation: -1373.0 m
Liman-7904 * Latitude: 43.300000 * Longitude: 29.966667 * Elevation: -1373.0 m * Location: Black Sea * Campaign: AKU26A * Basis: Akademik Kurchatov * Device: Multiple investigations (MULT)
Liman-7905 * Latitude: 43.333333 * Longitude: 30.500000 * Elevation: -1710.0 m * Location: Black Sea * Campaign: AKU26A * Basis: Akademik Kurchatov * Device: Multiple investigations (MULT)
|#||Name||Short Name||Unit||Principal Investigator||Method||Comment|
|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||Kondyurin, A V|
|6||Conductivity, thermal||k||W/m/K||Kondyurin, A V|
|7||Heat Flow||HF||mW/m2||Kondyurin, A V|
78 data points