(Table 1) Heat flow data in the western Black Sea
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| Autores principales: | , |
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| Formato: | Dataset Open Access |
| Lenguaje: | en |
| Publicado: |
PANGAEA
1983
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| _version_ | 1867171775031279616 |
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| author | Kondyurin, A V Sochel'nikov, V V |
| author_facet | Kondyurin, A V Sochel'nikov, V V |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | 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. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_755928 |
| institution | PANGAEA |
| language | en |
| publishDate | 1983 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | (Table 1) Heat flow data in the western Black Sea Kondyurin, A V Sochel'nikov, V V Akademik Kurchatov; AKU26A; Archive of Ocean Data; ARCOD; Black Sea; Conductivity, thermal; Elevation of event; Event label; Heat flow; Latitude of event; Liman-7904; Liman-7905; Liman-7906; Liman-7907; Liman-7908; Liman-7909; Liman-7910; Liman-7911; Liman-7912; Liman-7914; Liman-7915; Liman-7916; Liman-7928; Liman-7929; Liman-7930; Liman-7933; Liman-7934; Liman-7936; Liman-7938; Liman-7940; Liman-7945; Liman-7946; Liman-7948; Liman-7949; Liman-7950; Liman-7951; Longitude of event; MULT; Multiple investigations; Temperature (thermal) gradient 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. |
| title | (Table 1) Heat flow data in the western Black Sea |
| topic | Akademik Kurchatov; AKU26A; Archive of Ocean Data; ARCOD; Black Sea; Conductivity, thermal; Elevation of event; Event label; Heat flow; Latitude of event; Liman-7904; Liman-7905; Liman-7906; Liman-7907; Liman-7908; Liman-7909; Liman-7910; Liman-7911; Liman-7912; Liman-7914; Liman-7915; Liman-7916; Liman-7928; Liman-7929; Liman-7930; Liman-7933; Liman-7934; Liman-7936; Liman-7938; Liman-7940; Liman-7945; Liman-7946; Liman-7948; Liman-7949; Liman-7950; Liman-7951; Longitude of event; MULT; Multiple investigations; Temperature (thermal) gradient |
| url | https://doi.org/10.1594/PANGAEA.755928 |