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Ocean bottom hydrophone sgy-files of wide-angle seismic data of profile ATLAN...
Wide-Angle Seismic (WAS) data acquired across ATLANTIS-I profile in 2022 at 31ºN Central Atlantic. The seismic data were recorded with 22 ocean bottom hydrophones (OBH) from... -
Ocean bottom hydrophone sgy-files of wide-angle seismic data across the Xisha...
Wide-angle seismic data acquired across the Xisha Trough in the South China Sea. The data were acquired with 10 Ocean Bottom Hydrpobones from GEOMAR in 1996. The records are... -
Ocean bottom seismic data from the continent-ocean transition in the Deep Gal...
Seismic data was acquired to study the transition from rifted continental crust to oceanic crust at the Deep Galicia Margin from June to August 2013. 3D Multichannel reflection... -
Ocean bottom seismic data from the continent-ocean transition in the Deep Gal...
Seismic data was acquired to study the transition from rifted continental crust to oceanic crust at the Deep Galicia Margin from June to August 2013. 3D Multichannel reflection... -
Ocean bottom seismic data from the continent-ocean transition in the Deep Gal...
Seismic data was acquired to study the transition from rifted continental crust to oceanic crust at the Deep Galicia Margin from June to August 2013. 3D Multichannel reflection... -
Ocean bottom seismic data from the continent-ocean transition in the Deep Gal...
Seismic data was acquired to study the transition from rifted continental crust to oceanic crust at the Deep Galicia Margin from June to August 2013. 3D Multichannel reflection... -
Wide-angle seismic data from Sumatra
Ocean bottom seismometer data from the MD 156/Sumatra-OBS cruise (2006) During the Sumatra-OBS cruise (R/V Marion Dufresne, July–August 2006) 56 ocean bottom seismometers from... -
Crustal structure of the East-African Limpopo Margin, a strike-slip rifted co...
Coincident wide-angle and multi-channel seismic data acquired within the scope of the PAMELA Moz3-5 project allow to reconsider the formation mechanism of East-African margins...