Trace-element mobilization during Ca-metasomatism along a major fluid conduit: Eclogitization of blueschist as a consequence of fluid-rock interaction
In the subduction complex of the Tianshan mountains, western China, massive blueschist is cross-cut by an eclogite-facies major fluid conduit surrounded by a reaction zone which is mainly composed of omphacite and garnet. Petrological as well as geochemical evidence suggest that formation of the vei...
| Main Authors: | , , , |
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| Format: | Journal Article |
| Published: |
Pergamon
2010
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| Online Access: | http://hdl.handle.net/20.500.11937/5456 |