(Table 1) Heat flow measurements in the Black Sea
| Cobertura |
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 |
|---|---|
| Data(s) |
17/12/1980
|
| Resumo |
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. |
| Formato |
text/tab-separated-values, 80 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.755379 doi:10.1594/PANGAEA.755379 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Fonte |
Supplement to: Zolotarev, Vladimir G; Kobzar, VM (1980): New heat-flow measurements in the Black Sea. Oceanology, 20(1), 69-71 |
| Palavras-Chave | #Admiral Vladimirskiy; Archive of Ocean Data; ARCOD; AVL-1976; AVL-7601; AVL-7602; AVL-7603; AVL-7604; AVL-7605; Black Sea; Calculated; Conductivity, thermal; Elevation of event; Event label; GC; Gravity corer; Heat Flow; Heat Flow, standard deviation; Latitude of event; Longitude of event; Mikhail Lomonosov; ML35; ML35-3142; ML35-3149; ML35-3149a; ML35-3151; ML35-3153; ML35-3161; ML35-3168; ML35-3177; ML35-3187; ML35-3190; ML35-3197; ML35-3203; ML35-3204; ML35-3206; ML35-3207; Temperature (thermal) gradient; Thermistor |
| Tipo |
Dataset |
