Heat flow and heat transfer conditions in the bottom sediments of the equatorial indian ocean
The results are reported of heat flow determinations during the 10th and 11th cruises of the “Akademik Vernadsky”. Geothermal gradients were measured by the thermograd PTG-2MTB, with two temperature sensors of 1 or 1.2 m spacing. The temperature sensors were fixed to the coring tube. The lower senso...
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| Veröffentlicht in: | Geothermics 1979, Vol.8 (1), p.31-36 |
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| Hauptverfasser: | , , |
| Format: | Artikel |
| Sprache: | eng |
| Online-Zugang: | Volltext |
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