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author Villinger, Heinrich
Kaul, Norbert
Kuhn, Thomas
Müller, Paulina
author_facet Villinger, Heinrich
Kaul, Norbert
Kuhn, Thomas
Müller, Paulina
collection Datos científicos de ciencias marinas y ambientales
contents The heat flux measurements presented in this report were made during expedition SO240 on the German research vessel RV Sonne. The cruise started on the 3rd of may 2015 in Manzanillo (Mexico) and ended on the 16th of June 2015 in Manzanillo (Mexico). A total of 109 heat flux measurements were successfully carried out accompanied by detailed sediment echosounder and single channel seismic measurements on all heat flux profiles. 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 the measurements clearly showed that cold seawater enters the subsurface at one seamount investigated in detail, no diffuse leakage of hydrothermal fluids could be detected at any location.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_965467
institution PANGAEA
language en
publishDate 2024
publisher PANGAEA
record_format pangaea
spellingShingle Heat flux results of RV SONNE cruise SO240
Villinger, Heinrich
Kaul, Norbert
Kuhn, Thomas
Müller, Paulina
Calculated; Conductivity, thermal; DATE/TIME; Eastern Equatorial Pacific; ELEVATION; Event label; Heat flow; Heat-Flow probe; HF; LATITUDE; LONGITUDE; marine heat flow; North Pacific Ocean; Sensor, counts; SO240; SO240_12-1; SO240_20-1; SO240_24-1; SO240_3-1; SO240_32-1; SO240_36-1; SO240_45-1; SO240_52-1; SO240_56-1; SO240_60-1; SO240_67-1; SO240_7-1; SO240_71-1; SO240_77-1; SO240_87-1; SO240_92-1; SO240_94-1; Sonne_2; Station label; Temperature gradient
The heat flux measurements presented in this report were made during expedition SO240 on the German research vessel RV Sonne. The cruise started on the 3rd of may 2015 in Manzanillo (Mexico) and ended on the 16th of June 2015 in Manzanillo (Mexico). A total of 109 heat flux measurements were successfully carried out accompanied by detailed sediment echosounder and single channel seismic measurements on all heat flux profiles. 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 the measurements clearly showed that cold seawater enters the subsurface at one seamount investigated in detail, no diffuse leakage of hydrothermal fluids could be detected at any location.
title Heat flux results of RV SONNE cruise SO240
topic Calculated; Conductivity, thermal; DATE/TIME; Eastern Equatorial Pacific; ELEVATION; Event label; Heat flow; Heat-Flow probe; HF; LATITUDE; LONGITUDE; marine heat flow; North Pacific Ocean; Sensor, counts; SO240; SO240_12-1; SO240_20-1; SO240_24-1; SO240_3-1; SO240_32-1; SO240_36-1; SO240_45-1; SO240_52-1; SO240_56-1; SO240_60-1; SO240_67-1; SO240_7-1; SO240_71-1; SO240_77-1; SO240_87-1; SO240_92-1; SO240_94-1; Sonne_2; Station label; Temperature gradient
url https://doi.org/10.1594/PANGAEA.965467