The Majorite-Pyrope + Magnesiowüstite Assemblage: Constraints on the History of Shock Veins in Chondrites-Reference-Cited by-同舟云学术

The Majorite-Pyrope + Magnesiowüstite Assemblage: Constraints on the History of Shock Veins in Chondrites

Published:1996-03-15 Issue:5255 Volume:271 Page:1570-1573
ISSN:0036-8075
Container-title:Science
language:en
Short-container-title:Science

Author:

Chen Ming¹,Sharp Thomas G.²,Goresy Ahmed El³,Wopenka Brigitte⁴,Xie Xiande⁵

Affiliation:

1. M. Chen, Max-Planck-Institut für Kernphysik, Saupfercheckweg 1, D-69117 Heidelberg, Germany, and Guangzhou Institute of Geochemistry, Academia Sinica, 510640 Guangzhou, China.

2. T. G. Sharp, Bayerisches Geoinstitut, Universität Bayreuth, D-95440 Bayreuth, Germany.

3. A. El Goresy, Max-Planck-Institut für Kernphysik, Saupfercheckweg 1, D-69117 Heidelberg, Germany.

4. B. Wopenka, Department of Earth and Planetary Sciences, Washington University, St. Louis, MO 63130, USA.

5. X. Xie, Guangzhou Institute of Geochemistry, Academia Sinica, 510640 Guangzhou, China.

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

Reference40 articles.

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4. STRUCTURE AND TWINNING OF SINGLE-CRYSTAL MGSIO3 GARNET SYNTHESIZED AT 17 GPA AND 1800-DEGREES-C;ANGEL J. R.;AMERICAN MINERALOGIST,1989

5. MECHANISMS OF THE TRANSFORMATIONS BETWEEN THE ALPHA-POLYMORPHS, BETA-POLYMORPHS AND GAMMA-POLYMORPHS OF MG2SIO4 AT 15 GPA;BREARLEY J. A.;PHYSICS AND CHEMISTRY OF MINERALS,1992

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