Os isotopic evidence for a carbonaceous chondritic mantle source for the Nagqu ophiolite from Tibet and its implications
Author:
Publisher
Springer Science and Business Media LLC
Subject
Multidisciplinary
Link
http://link.springer.com/content/pdf/10.1007/s11434-012-5384-8.pdf
Reference86 articles.
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3. Dilek Y, Moores E M, Elthon D, et al. Ophiolites and Oceanic Crust: New Insights from Field Studies and the Ocean Drilling Program. Boulder: Geological Society of America Special Paper, 2000
4. Shirey S B, Walker R J. The Re-Os isotope system in cosmochemistry and high-temperature geochemistry. Ann Rev Earth Planet Sci, 1998, 26: 423–500
5. Zhi X C. Re-Os isotopic system and formation age of subcontinental lithosphere mantle. Chin Sci Bull, 2000, 45: 193–200
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