期刊文献+

Xieite,a new mineral of high-pressure FeCr_2O_4 polymorph 被引量:9

Xieite,a new mineral of high-pressure FeCr_2O_4 polymorph
原文传递
导出
摘要 Xieite,a new mineral,occurs in the shock vein of the Suizhou meteorite.The mineral has an ortho-rhombic structure and its space group is Bbmm.The cell parameters are a = 9.462(6),b = 9.562(9),c = 2.916(1).The crystal-chemical formula is(Fe0.87Mg0.13Mn0.01)1.01(Cr1.62Al0.25Ti0.08V0.02)1.97O4,or simply formula FeCr2O4.Stronger X-ray diffraction lines are [d(),I/Io]:(2.675,100),(2.389,20),(2.089,10),(1.953,90),(1.566,60),(1.439,15),(1.425,15),(1.337,40).Xieite is a high pressure polymorph of FeCr2O4 and formed by solid-state transformation of chromite under shock-induced high pressure and tem-perature,in association with other high-pressure minerals including ringwoodite,majorite,lingunite and tuite.The P-T condition for the formation of xieite is estimated to be 18―23 GPa and 1800―1950℃,respectively.Xieite has recently been approved by the Commission on New Minerals,Nomenclature and Classification of the International Mineralogical Association(IMA 2007-056).The mineral name,xieite,is named after Xiande Xie. Xieite, a new mineral, occurs in the shock vein of the Suizhou meteorite. The mineral has an orthorhombic structure and its space group is Bbmm. The cell parameters are a = 9.462(6) A, b = 9.562(9) A, c = 2.916(1)A. The crystal-chemical formula is (Fe0.87Mg0.13Mn0.01)1.01(Cr1.62AI0.25Ti0.08V0.02)1.97O4, or simply formula FeCr2O4. Stronger X-ray diffraction lines are [d (A), I/Io]: (2.675, 100), (2.389, 20), (2.089, 10), (1.953, 90), (1.566, 60), (1.439, 15), (1.425, 15), (1.337, 40). Xieite is a high pressure polymorph of FeCr2O4 and formed by solid-state transformation of chromite under shock-induced high pressure and temperature, in association with other high-pressure minerals including ringwoodite, majorite, lingunite and tuite. The P-Tcondition for the formation of xieite is estimated to be 18--23 GPa and 1800--1950℃, respectively. Xieite has recently been approved by the Commission on New Minerals, Nomenclature and Classification of the International Mineralogical Association (IMA 2007-056). The mineral name, xieite, is named after Xiande Xie.
出处 《Chinese Science Bulletin》 SCIE EI CAS 2008年第21期3341-3345,共5页
基金 National Natural Science Foundation of China (Grant Nos. 40672035 and 40272028) the Chinese Academy of Sciences (Grant No. KJCX2-SW-N20)
关键词 络铁矿 高压环境 基因多态性 矿物 xieite, chromite, high-pressure, polymorph, new mineral, shock, Suizhou meteorite
  • 相关文献

参考文献11

  • 1D. Andrault,N. Bolfan-Casanova.High-pressure phase transformations in the MgFe2O4 and Fe2O3–MgSiO3 systems[J].Physics and Chemistry of Minerals.2001(3)
  • 2Bertaut E F,,Blum P.Determination de la Structure de Ti2CaO4 par la Méthode Self-Consistante d’Approche Directe[].Acta Crystallographica.1956
  • 3Bright N F H,Rowland J F,Wurm J G.The compound CaO.Ti2O3[].Canadian Journal of Chemistry.1958
  • 4Chen M,Sharp T G,El Goresy A, et al.The majorite-pyrope + mag- nesiowstite assemblage: constraints on the history of shock veins in chondrites[].Science.1996
  • 5Green H W II.Shock-induced minerals in meteorite provide pros- pecting tools for mineral physics[].Proceedings of the National Academy of Sciences of the United States of America.2004
  • 6Gillet P,Chen M. (,Dubrovinsky L,and El Goresy A. (.Natural NaAlSi3O(?)-hollandite in the shocked Sixiangkou meteorite[]."Science".2000
  • 7C.B. Agee,J. Li,M.C. Shannon,S. Circone.Pressure–temperature phase diagram for the Allende meteorite[].Journal of Geophysical Research.1995
  • 8Chen Ming,Shu Jinfu,Mao Ho-kwang,et al.Naatural occurrence and synthesis of two new postspinel polymorphs of chromite[].Proceedings of the National Academy of Sciences of the United States of America.2003
  • 9Reid AF and Ringwood AE.[].Earth and Planetary Science.1969
  • 10Irifune T,Fujino K and Ohtani E.[].Nature.1991

同被引文献167

引证文献9

二级引证文献30

相关作者

内容加载中请稍等...

相关机构

内容加载中请稍等...

相关主题

内容加载中请稍等...

浏览历史

内容加载中请稍等...
;
使用帮助 返回顶部