Alkaline fluid circulation in ultramafic rocks and formation of nucleotide constituents: a hypothesis
<p>Abstract</p> <p>Seawater is constantly circulating through oceanic basement as a low-temperature hydrothermal fluid (<150°C). In cases when ultramafic rocks are exposed to the fluids, for instance during the initial phase of subduction, ferromagnesian minerals are altered in...
| Main Authors: | , , , |
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| Format: | Article |
| Language: | English |
| Published: |
BMC
2006-07-01
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| Series: | Geochemical Transactions |
| Online Access: | http://www.geochemicaltransactions.com/content/7/1/7 |