Geothermal flow in the western part of the Black Sea.
- DSpace Home
- →
- Геология России
- →
- PANGAEA
- →
- View Item
JavaScript is disabled for your browser. Some features of this site may not work without it.
dc.contributor.author | Kondyurin, A V | |
dc.contributor.author | Sochel'nikov, V V | |
dc.coverage.spatial | 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 | |
dc.date.accessioned | 2019-11-23T11:53:58Z | |
dc.date.available | 2019-11-23T11:53:58Z | |
dc.date.issued | 1983-01-17 | |
dc.identifier | https://doi.pangaea.de/10.1594/PANGAEA.755928 | |
dc.identifier | https://doi.org/10.1594/PANGAEA.755928 | |
dc.identifier.citation | Kondyurin, A V; Sochel'nikov, V V (1983): Geothermal flow in the western part of the Black Sea. Oceanology, 23(4), 468-472 | |
dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/7351 | |
dc.description.abstract | 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. | |
dc.format | text/tab-separated-values, 78 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: Kondyurin, A V; Sochel'nikov, V V (1983): Geothermal flow in the western part of the Black Sea. Oceanology, 23(4), 468-472 | |
dc.subject | Akademik Kurchatov | |
dc.subject | AKU26A | |
dc.subject | Archive of Ocean Data | |
dc.subject | ARCOD | |
dc.subject | Black Sea | |
dc.subject | Conductivity, thermal | |
dc.subject | Heat flow | |
dc.subject | Liman-7904 | |
dc.subject | Liman-7905 | |
dc.subject | Liman-7906 | |
dc.subject | Liman-7907 | |
dc.subject | Liman-7908 | |
dc.subject | Liman-7909 | |
dc.subject | Liman-7910 | |
dc.subject | Liman-7911 | |
dc.subject | Liman-7912 | |
dc.subject | Liman-7914 | |
dc.subject | Liman-7915 | |
dc.subject | Liman-7916 | |
dc.subject | Liman-7928 | |
dc.subject | Liman-7929 | |
dc.subject | Liman-7930 | |
dc.subject | Liman-7933 | |
dc.subject | Liman-7934 | |
dc.subject | Liman-7936 | |
dc.subject | Liman-7938 | |
dc.subject | Liman-7940 | |
dc.subject | Liman-7945 | |
dc.subject | Liman-7946 | |
dc.subject | Liman-7948 | |
dc.subject | Liman-7949 | |
dc.subject | Liman-7950 | |
dc.subject | Liman-7951 | |
dc.subject | MULT | |
dc.subject | Temperature (thermal) gradient | |
dc.title | Geothermal flow in the western part of the Black Sea. | |
dc.title.alternative | (Table 1) Heat flow data in the western Black Sea | |
dc.type | Dataset |
Files in this item
Files | Size | Format | View |
---|---|---|---|
There are no files associated with this item. |
This item appears in the following Collection(s)
-
PANGAEA
Метаданные публикаций с сайта https://www.pangaea.de/