Is there an active hydrothermal flux from the Orca seamount in the Bransfield Strait, Antarctica?
The rifting zone of Bransfield Strait, Antarctica, is tectonically and geologically unique. It is a back-arc basin that was opened by extensional forces associated to roll-back subduction after cessation of spreading activity of the Phoenix Ridge, and the transtension of the westward ending of Scoti...
Published in: | Andean Geology |
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Main Authors: | , , , |
Other Authors: | , , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
HAL CCSD
2018
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Subjects: | |
Online Access: | https://hal.sorbonne-universite.fr/hal-01958159 https://hal.sorbonne-universite.fr/hal-01958159/document https://hal.sorbonne-universite.fr/hal-01958159/file/3086-11559-1-PB_sans%20marque.pdf https://doi.org/10.5027/andgeoV45n3-3086 |