Delamination of Continental Lithosphere Beneath an Active Margin? Thermobarometric and Rhenium-Osmium-Isotopic Constraints from Sierra Nevadan Xenoliths

Details Delamination of Continental Lithosphere Beneath an Active Margin? Thermobarometric and Rhenium-Osmium-Isotopic Constraints from Sierra Nevadan Xenoliths Delamination of Continental Lithosphere Beneath an Active Margin? Thermobarometric and Rhenium-Osmium-Isotopic Constraints from Sierra Nevadan Xenoliths

Aug 1999

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1999nag..conf.7645l&link_type=article

Ninth Annual V. M. Goldschmidt Conference, August 22-27, 1999, Cambridge, Massachusetts, abstract no. 7645

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