Temperature vs depth profile at heat flux station HF1760 of RV MARIA S. MERIAN cruise MSM69
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| Auteurs principaux: | , , , |
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| Format: | Dataset Open Access |
| Langue: | en |
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PANGAEA
2025
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| _version_ | 1867170436160159744 |
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| author | Villinger, Heinrich Grevemeyer, Ingo Kaul, Norbert Singh, Satish C |
| author_facet | Villinger, Heinrich Grevemeyer, Ingo Kaul, Norbert Singh, Satish C |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | The heat flux measurements presented in this report were made during expedition MSM69 on the German research vessel RV Maria S. Merian (November 14, 2017 to December 22, 2017). A total of 69 heat flux measurements (profile HF1760 to profile HF1767) were successfully carried out colocated with the iLAB reflexion seismic profile. The aim of the measurements was to investigate whether low-temperature hydrothermal fluids diffuse at the seafloor where the oceanic basement is not covered by sediments. While low heat flux measurements clearly show that cold seawater enters the subsurface, no diffuse leakage of hydrothermal fluids could be detected at any location. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_980094 |
| institution | PANGAEA |
| language | en |
| publishDate | 2025 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | Temperature vs depth profile at heat flux station HF1760 of RV MARIA S. MERIAN cruise MSM69 Villinger, Heinrich Grevemeyer, Ingo Kaul, Norbert Singh, Satish C Conductivity, thermal; DEPTH, sediment/rock; Eastern Equatorial Atlantic; Heat flow probe; Heat-Flow probe; heat flux; HF; HF1760; iLAB seismic profile; Maria S. Merian; MSM69; MSM69_6-1; Sensor, number; Station label; Temperature, in rock/sediment The heat flux measurements presented in this report were made during expedition MSM69 on the German research vessel RV Maria S. Merian (November 14, 2017 to December 22, 2017). A total of 69 heat flux measurements (profile HF1760 to profile HF1767) were successfully carried out colocated with the iLAB reflexion seismic profile. The aim of the measurements was to investigate whether low-temperature hydrothermal fluids diffuse at the seafloor where the oceanic basement is not covered by sediments. While low heat flux measurements clearly show that cold seawater enters the subsurface, no diffuse leakage of hydrothermal fluids could be detected at any location. |
| title | Temperature vs depth profile at heat flux station HF1760 of RV MARIA S. MERIAN cruise MSM69 |
| topic | Conductivity, thermal; DEPTH, sediment/rock; Eastern Equatorial Atlantic; Heat flow probe; Heat-Flow probe; heat flux; HF; HF1760; iLAB seismic profile; Maria S. Merian; MSM69; MSM69_6-1; Sensor, number; Station label; Temperature, in rock/sediment |
| url | https://doi.org/10.1594/PANGAEA.980094 |