Deep high-temperature hydrothermal circulation in a detachment faulting system on the ultra-slow spreading ridge
Magmatic and tectonic activity at mid-oceanic ridges can give detailed insights into high-temperature hydrothermal circulation of fluids. The authors here present geochemical and geophysical datasets that suggest a hydrothermal system penetrating the upper lithospheric mantle at an ultra-slow spread...
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| Auteurs principaux: | , , , , , , , , , , , , , , , , , , , , , |
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| Format: | article |
| Langue: | EN |
| Publié: |
Nature Portfolio
2020
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| Accès en ligne: | https://doaj.org/article/292c393ebaf04e258ce492c5da96b6b2 |
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