Gas hydrates of nonpressurized (GC) and pressurized (DAPC) sediment cores from the Hakon Mosby Mud Volcano, SW Barents Sea

The occurrence of gas hydrates at submarine mud volcanoes (MVs) located within the gas hydrate stability zone (GHSZ) is controlled by upward fluid and heat flux associated with MV activity. Determining the spatial distribution of gas hydrates at MVs is crucial to evaluate their sensitivity to known...

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Bibliographic Details
Main Authors: Pape, Thomas, Feseker, Tomas, Kasten, Sabine, Fischer, David, Bohrmann, Gerhard
Format: Dataset
Language:English
Published: PANGAEA 2011
Subjects:
GC
PC
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.770365
https://doi.org/10.1594/PANGAEA.770365