RINGWOODITE RIMS AROUND OLIVINE CORES IN SHOCK-INDUCED MELT VEINS OF AN ANTARCTIC CHONDRITE: MECHANISMS OF TRANSFORMATION AND FE-MG DIFFUSION

被引:0
|
作者
Xie, Z. [1 ]
Li, X. [1 ]
Sharp, T. G. [2 ]
De Carli, P. S. [3 ]
机构
[1] Nanjing Univ, Nanjing 210008, Peoples R China
[2] Arizona State Univ, Tempe, AZ 85287 USA
[3] SRI Int, Menlo Pk, CA 94025 USA
关键词
HIGH-PRESSURE MINERALS; L6; CHONDRITE; CONSTRAINTS; PHASES;
D O I
暂无
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
引用
收藏
页码:A219 / A219
页数:1
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    Sharp, Thomas G.
    Leinenweber, Kurt
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    [J]. AMERICAN MINERALOGIST, 2011, 96 (2-3) : 430 - 436
  • [4] Natural occurrence of a new mineral with an olivine structure and pyroxene composition in the shock-induced melt veins of Tenham L6 chondrite
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    [J]. METEORITICS & PLANETARY SCIENCE, 2008, 43 (07) : A170 - A170
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