- Abstract:
-
This study presents major-, trace-element, and rhenium-osmium (Re-Os) isotope and elemental data for basalts and gabbros from the Zermatt-Saas ophiolite, metamorphosed to eclogite-facies conditions during the Alpine orogeny. Igneous crystallisation of the gabbros occurred at 163.5 ± 1.8 Ma and both gabbro and basalt were subject to 'peak' pressure-temperature (P-T) conditions of > 2.0 GPa and ~ 600 °C at about 40.6 ± 2.6 Ma. Despite such extreme P-T conditions, Re-Os isotope and abundance ...
Expand abstract - Publication status:
- Published
- Publisher copy:
- 10.1016/j.epsl.2006.10.029
-
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- Journal:
- EARTH AND PLANETARY SCIENCE LETTERS
- Volume:
- 253
- Issue:
- 1-2
- Pages:
- 211-225
- Publication date:
- 2007-01-15
- DOI:
- ISSN:
-
0012-821X
- URN:
-
uuid:3fb67e89-aed8-407c-b66b-e8993325b6e2
- Source identifiers:
-
152072
- Local pid:
- pubs:152072
- Keywords:
- Copyright date:
- 2007
Journal article
Rhenium-osmium isotope and elemental behaviour during subduction of oceanic crust and the implications for mantle recycling
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