Tracing fluid-rock reaction and hydrothermal circulation at the Saldanha hydrothermal field
The Saldanha hydrothermal field is positioned on the top of a seamount located in a non-transformoffset (NTO5) on the Mid-Atlantic Ridge (MAR). This hydrothermal system was first described as a low-temperature diffuse field, driven by peridotite-seawater reactions following the detection of high con...
| Main Authors: | , , , , , , |
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| Format: | Article |
| Language: | English |
| Published: |
2010-05-15.
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| Subjects: | |
| Online Access: | Get fulltext |