Non-cratonic Diamonds from UHP Metamorphic Terranes, Ophiolites and Volcanic Sources

Author:

Dobrzhinetskaya Larissa F.1,O’Bannon Earl F.2,Sumino Hirochika3

Affiliation:

1. Department of Earth and Planetary Sciences, University of California at Riverside, 900 University Ave, Riverside, CA 92521, USA

2. Physical and Life Sciences, Physics Division, Lawrence Livermore National Laboratory, Livermore, CA 94550, USA

3. Department of General Systems Studies, Graduate School of Arts and Science, University of Tokyo, 3-8-1 Komaba, Tokyo, Japan

Publisher

Mineralogical Society of America

Subject

Geochemistry and Petrology

Reference346 articles.

1. Crystallization of diamond from C–O–H fluids under high-pressure and high-temperature conditions;Akaishi;J Cryst Growth,2000

2. Constraints on evolution of Earth’s mantle from rare gas systematics;Allègre;Nature,1983

3. Properties of diamond with varying isotopic composition;Anthony;Diam Relat Mater,1992

4. Conversion of low–pressure chromitites to ultrahigh-pressure chromitites by deep recycling: a good inference;Arai;Earth Planet Sci Lett,2013

5. The types andcharacteristics of basic and ultrabasic rocks from China;Bai;Bull Inst Geol Chin Acad Geol Sci (in Chinese),1989

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