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...
| Published in: | Biogeosciences |
|---|---|
| Main Authors: | , , , , , , , , , , , , , |
| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2018-09-01
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| Online Access: | https://www.biogeosciences.net/15/5715/2018/bg-15-5715-2018.pdf |