ADVANCES IN POLAR SCIENCE ›› 2013, Vol. 25 ›› Issue (4): 378-385.DOI: 10.3724/SP.J.1084.2013.00378

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THE STUDY OF AND EXPECTATIONS FOR FINDING CARBONACEOUS CHONDRITES IN THE GROVE MOUNTAINS, ANTARCTICA

DAI Deqiu1,2,CHEN Xinyue1,Yang Rongfeng1,3   

  1.  
    1Institute of Geology, Hunan University of Science and Technology, Xiangtan 411201, China;
    2Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550002, China;
    3Hunan Provincial Key Laboratory of Shale Gas Resource Utilization, Xiangtan 411201, China
  • Received:2013-04-03 Revised:2013-04-12 Online:2013-12-30 Published:2013-12-30

Abstract: Petrography and mineral chemistry of 3 carbonaceous chondrites (GRV 020025, 021579 and 022459) collected from the Grove Mountains (GRV), Antarctica, were reported here. All 3 chondrites are unequilibrated.The modal abundance ratio of matrix/chondrule are 2.8 (GRV 020025), 1.2 (GRV 021579) and 1 (GRV 022459). GRV 022459 has the largest chondrules (0.6-2.0 mm). A total 27 Ca-, Al-rich inclusions have been found in the three chondrites. Except for one spinel-spherule in each GRV 020025 and 021579, all other inclusions can be classified as Type A (or Type A-like) or spinel-pyroxene-rich inclusions. Most of the inclusions are intensively altered, with abundant phyllosilicates in the inclusions from GRV 020025 and FeO-enrichment of spinel in GRV 022459. At last, we look forward to the step studying work of Antarctica carbonaceous chondrites.

Key words: petrography and mineral chemistry, Ca-, Al-rich inclusions, carbonaceous chondrites, Antarctica