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Main Authors: Villinger, Heinrich, Grevemeyer, Ingo, Kaul, Norbert, Singh, Satish C
Format: Dataset Open Access
Language:en
Published: PANGAEA 2025
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Online Access:https://doi.org/10.1594/PANGAEA.980483
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_version_ 1867172206165884928
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_980483
institution PANGAEA
language en
publishDate 2025
publisher PANGAEA
record_format pangaea
spellingShingle Temperature vs depth profile at heat flux station HF1761 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; HF1761; iLAB seismic profile; Maria S. Merian; MSM69; MSM69_19-1; 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 HF1761 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; HF1761; iLAB seismic profile; Maria S. Merian; MSM69; MSM69_19-1; Sensor, number; Station label; Temperature, in rock/sediment
url https://doi.org/10.1594/PANGAEA.980483