On the formation of hydrothermal vents and cold seeps in the Guaymas Basin, Gulf of California

<p>Magmatic sill intrusions into organic-rich sediments cause the release of thermogenic CH<sub>4</sub> and CO<sub>2</sub>. Pore fluids from the Guaymas Basin (Gulf of California), a sedimentary basin with recent magmatic activity, were investigated to constrain the...

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Main Authors: S. Geilert, C. Hensen, M. Schmidt, V. Liebetrau, F. Scholz, M. Doll, L. Deng, A. Fiskal, M. A. Lever, C.-C. Su, S. Schloemer, S. Sarkar, V. Thiel, C. Berndt
Format: Article
Language:English
Published: Copernicus Publications 2018-09-01
Series:Biogeosciences
Online Access:https://www.biogeosciences.net/15/5715/2018/bg-15-5715-2018.pdf