The majorite-pyrope + magnesiowüstite assemblage: Constraints on the history of shock veins in chondrites

Science

Volumn 271, Issue 5255, 1996, Pages 1570-1573

  Chen, Ming ^a,b   Sharp, Thomas G ^c   El Goresy, Ahmed ^a   Wopenka, Brigitte ^d   Xie, Xiande ^b  

^a MAX PLANCK INSTITUT FÜR KERNPHYSIK   (Germany)

^b GUANGZHOU INSTITUTE OF GEOCHEMISTRY   (China)

^c UNIVERSITÄT BAYREUTH   (Germany)

^d WASHINGTON UNIVERSITY   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

CHONDRITE L6; MAGNESIOWUSTITE; MAJORITE; PYROPE; SHOCK VEIN; SIXIANGKOV METEORITE;

EID: 0029752404     PISSN: 00368075     EISSN: None     Source Type: Journal    
DOI: 10.1126/science.271.5255.1570     Document Type: Article

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43. 5 , 6.02 Fe, 1.21 Ni, and 6.00 FeS; total, 99.37 weight %
44. B.W. was supported by NSF grant GER 9023520.