New heat-flow measurements in the Black Sea.
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dc.contributor.author | Zolotarev, Vladimir G | |
dc.contributor.author | Kobzar, V M | |
dc.coverage.spatial | MEDIAN LATITUDE: 42.837500 * MEDIAN LONGITUDE: 35.134167 * SOUTH-BOUND LATITUDE: 41.700000 * WEST-BOUND LONGITUDE: 30.366667 * NORTH-BOUND LATITUDE: 43.666667 * EAST-BOUND LONGITUDE: 39.600000 * MINIMUM ELEVATION: -2220.0 m * MAXIMUM ELEVATION: -1920.0 m | |
dc.date.accessioned | 2019-11-23T11:53:58Z | |
dc.date.available | 2019-11-23T11:53:58Z | |
dc.date.issued | 1980-12-17 | |
dc.identifier | https://doi.pangaea.de/10.1594/PANGAEA.755379 | |
dc.identifier | https://doi.org/10.1594/PANGAEA.755379 | |
dc.identifier.citation | Zolotarev, Vladimir G; Kobzar, V M (1980): New heat-flow measurements in the Black Sea. Oceanology, 20(1), 69-71 | |
dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/7350 | |
dc.description.abstract | New data show that the thermal field is definitely related to the geologic structure at depth and to other geophysical fields. Low heat-flow values along reliably established subsurface faults suggest absence of a heated zone of the earth's crust and upper mantle in these regions. | |
dc.format | text/tab-separated-values, 80 data points | |
dc.language.iso | en | |
dc.publisher | PANGAEA | |
dc.rights | CC-BY-3.0: Creative Commons Attribution 3.0 Unported | |
dc.rights | Access constraints: unrestricted | |
dc.source | Supplement to: Zolotarev, Vladimir G; Kobzar, V M (1980): New heat-flow measurements in the Black Sea. Oceanology, 20(1), 69-71 | |
dc.subject | Admiral Vladimirskiy | |
dc.subject | Archive of Ocean Data | |
dc.subject | ARCOD | |
dc.subject | AVL-1976 | |
dc.subject | AVL-7601 | |
dc.subject | AVL-7602 | |
dc.subject | AVL-7603 | |
dc.subject | AVL-7604 | |
dc.subject | AVL-7605 | |
dc.subject | Black Sea | |
dc.subject | Conductivity, thermal | |
dc.subject | GC | |
dc.subject | Gravity corer | |
dc.subject | Heat flow | |
dc.subject | Heat flow, standard deviation | |
dc.subject | Mikhail Lomonosov | |
dc.subject | ML35 | |
dc.subject | ML35-3142 | |
dc.subject | ML35-3149 | |
dc.subject | ML35-3149a | |
dc.subject | ML35-3151 | |
dc.subject | ML35-3153 | |
dc.subject | ML35-3161 | |
dc.subject | ML35-3168 | |
dc.subject | ML35-3177 | |
dc.subject | ML35-3187 | |
dc.subject | ML35-3190 | |
dc.subject | ML35-3197 | |
dc.subject | ML35-3203 | |
dc.subject | ML35-3204 | |
dc.subject | ML35-3206 | |
dc.subject | ML35-3207 | |
dc.subject | Temperature (thermal) gradient | |
dc.subject | Thermistor | |
dc.title | New heat-flow measurements in the Black Sea. | |
dc.title.alternative | (Table 1) Heat flow measurements in the Black Sea | |
dc.type | Dataset |
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