Lithium and its isotopes as tracers of subduction zone fluids and metasomatic processes: Evidence from the Catalina Schist, California, USA
The Catalina Schist, well-studied for its tectonometamorphic history and geochemical evolution, provides a field area in which to evaluate the extent of Li mobility in subduction-zone fluids and the degree to which Li isotopes can trace metamorphic fluid-rock interactions. A suite of 63 samples of t...
| Príomhchruthaitheoirí: | , , , , |
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| Formáid: | Journal article |
| Foilsithe / Cruthaithe: |
2012
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