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Grove Mountains (GRV) 024237: A New Ureilite from Antarctica

【标题】Grove Mountains (GRV) 024237: A New Ureilite from Antarctica

【Title】Grove Mountains (GRV) 024237: A New Ureilite from Antarctica

【DOI】10.3724/SP.J.1085.2012.00025

【作者】 王桂琴; 王道德; 缪秉魁

【Author】 Wang Guiqin ; Wang Daode ; Miao Bingkui

【期刊】极地研究

【Journal】ADVANCES IN POLAR SCIENCE

【期刊年份】2012

【卷】23

【期】1

【关键词】 Antarctic meteorite; ureilite; petrology; chemical composition; classification

【Keywords】 Antarctic meteorite; ureilite; petrology; chemical composition; classification

【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 Mountains,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.

【Abstract】 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 Mountains,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.

【基金/项目】 高精度Mg同位素组成对CAIs和球粒的成因制约和在地幔岩与陨石中的对比 ; 20100208

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