期刊文献+

Grove Mountains (GRV) 024237: A new ureilite from Antarctica 被引量:1

Grove Mountains (GRV) 024237: A new ureilite from Antarctica
下载PDF
导出
摘要 Ureilites share the characteristics of differentiated meteorites and of primary chondrites. GRV 024237 is a ureilite, which was found in the 19th Chinese National Antarctic Research Expedition (CHINARE), at the No. 4 moraine, Grove Moun- tains, Antarctica. GRV 024237 consists mainly of coarse-grained olivine (60 vol%), pigeonite (30 vol%) and opaque minerals (10 vol% ). Tri-junction texture between olivine and pigeonite is common. Carbonaceous materials with minor amounts of troilite and nickel-iron metal were observed as interstitial phases. The Fa value of olivine composition varies from 6.2 to 16.8 from rim to core, but pyroxene is homogeneous in composition, with Fs 14.0 to 15.5. Both olivine and pyroxene have normal extinctions. Net-like iron or limonite veins filled in the fractures of olivine and pyroxene, and no diamond was observed. Based on petrographic and mineralogical features, GRV 024237 is a Type I and Group 2 monomict ureilite. Ureilites share the characteristics of differentiated meteorites and of primary chondrites. GRV 024237 is a ureilite, which was found in the 19th Chinese National Antarctic Research Expedition (CHINARE), at the No. 4 moraine, Grove Moun- tains, Antarctica. GRV 024237 consists mainly of coarse-grained olivine (60 vol%), pigeonite (30 vol%) and opaque minerals (10 vol% ). Tri-junction texture between olivine and pigeonite is common. Carbonaceous materials with minor amounts of troilite and nickel-iron metal were observed as interstitial phases. The Fa value of olivine composition varies from 6.2 to 16.8 from rim to core, but pyroxene is homogeneous in composition, with Fs 14.0 to 15.5. Both olivine and pyroxene have normal extinctions. Net-like iron or limonite veins filled in the fractures of olivine and pyroxene, and no diamond was observed. Based on petrographic and mineralogical features, GRV 024237 is a Type I and Group 2 monomict ureilite.
出处 《Advances in Polar Science》 2012年第1期25-29,共5页 极地科学进展(英文版)
基金 supported by the Pilot Project of Knowledge Innovation Program of the Chinese Academy of Sciences (Grant no.kzcx2-yw-Q08) the National Natural Science Foundation of China (Grant no.40873054) the China Program for International Polar Year 2007-2008 the Polar Research Strategic Research Foundation of China (Grant no.20100208)
关键词 Antarctic meteorite ureilite PETROLOGY chemical composition CLASSIFICATION Antarctic meteorite, ureilite, petrology, chemical composition, classification
  • 相关文献

参考文献3

二级参考文献108

  • 1梁英,王鹤年,徐伟彪,季峻峰.南极GRV021788橄辉无球粒陨石的岩石学和矿物学特征[J].地球化学,2006,35(1):19-26. 被引量:9
  • 2王道德,缪秉魁,林杨挺.我国南极橄辉无球粒陨石(GRV 024516)和H5球粒陨石(GRV 024517)宇宙射线暴露年龄和气体保存年龄[J].极地研究,2006,18(3):157-165. 被引量:5
  • 3Grossman J N. The Meteofitical Bulletin, No. 83, 1999 Jtdy[J] .Meteorit Planet Sci, 1999, 34:A169 - A186.
  • 4Grossman J N. The Meteoritical Bulletin, No. 84, 2000 August[J]. Meteorit Planet Sci, 2000, 35:A199-A225.
  • 5Grossman J N, Zipfel J. The Meteoritical Bulletin, No. 85, 2001 September[J]. Meteorit Planet Sci, 2001, 36:A293-A322.
  • 6Goodrich C A. Ureilites: A critical review[J]. Meteoritics, 1992,27(4): 327-352.
  • 7Goodrich C A. Are ureilites residues from partial melting of ehondritic material? The answer from MAGPOX[J] . Meteorit Planet Sci, 1999, 34(1): 109-119.
  • 8Grossman J N. The Meteoritical Bulletin, No. 82, 1998 July[J].Meteorit Planet Sci, 1998, 33(4, suppl): A221-A239.
  • 9Russell S S, Folco L, Grady M M, Zolensky M E, Jones R,Righter K, Zipfel J, Gmssman J N. The Meteoritical Bulletin,No. 88, 2004 July[J] . Meteorit Planet Sci, 2004, 39(suppl):215 - 278.
  • 10Takeda H. Mineralogy of Antarctic ureilites and a working hypothesis for their origin and evolution[J]. Earth Planet Sci Eett,1987, 81(4): 358-370.

共引文献10

同被引文献69

引证文献1

二级引证文献3

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