Petrography and mineral chemistry of 4 carbonaceous chondrites from the Grove Mountains,Antarctica  被引量:2

Petrography and mineral chemistry of 4 carbonaceous chondrites from the Grove Mountains,Antarctica

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作  者:戴德求 王道德 

机构地区:[1]Institute of Geology,Hunan University of Science and Technology [2]Guangzhou Institute of Geochemistry,Chinese Academy of Sciences

出  处:《Chinese Journal of Polar Science》2009年第2期166-171,共6页极地研究(英文版)

基  金:supported by the Doctor's Foundation of Hunan University of Science and Technology(Grant No.E50806)

摘  要:Petrography and mineral chemistry of four carbonaceous chondrites ( GRV 020017, GRV 020025, GRV 021579, GRV 022459 ) collected from the Grove Mountains ( GRV), Antarctica, were reported here. All four chondrites are unequilibrated, as indicated by well shaped chondrules and the chemical variations of olivine and low-Ca pyroxene. The modal abundance ratio of matrix/chondrule are 2 ( GRV 020017), 2. 8 ( GRV 020025 ), l. 2 ( GRV 021579 ), 1 ( GRV 022459 ). GRV 022459 has the largest chondrules (0.6--2.0 ram). A total of 30 Ca-Al-rich inclu- sions were found in the four meteorites. Most inclusions were highly altered, with a- bundant phyllosilicates in the inclusions of GRV 020017 and GRV 020025. On the base of petrography and mineral chemistry, these chondrites are classified as CM2 (GRV 020017 and 020025), CO3 (GRV 021579) and CV3 (GRV 022459).Petrography and mineral chemistry of four carbonaceous chondrites ( GRV 020017, GRV 020025, GRV 021579, GRV 022459 ) collected from the Grove Mountains ( GRV), Antarctica, were reported here. All four chondrites are unequilibrated, as indicated by well shaped chondrules and the chemical variations of olivine and low-Ca pyroxene. The modal abundance ratio of matrix/chondrule are 2 ( GRV 020017), 2. 8 ( GRV 020025 ), l. 2 ( GRV 021579 ), 1 ( GRV 022459 ). GRV 022459 has the largest chondrules (0.6--2.0 ram). A total of 30 Ca-Al-rich inclu- sions were found in the four meteorites. Most inclusions were highly altered, with a- bundant phyllosilicates in the inclusions of GRV 020017 and GRV 020025. On the base of petrography and mineral chemistry, these chondrites are classified as CM2 (GRV 020017 and 020025), CO3 (GRV 021579) and CV3 (GRV 022459).

关 键 词:carbaonaceous chondrites petrography and mineral chemistry CAI CLASSIFICATION Antarctica. 

分 类 号:P185.83[天文地球—天文学] TD163.1[矿业工程—矿山地质测量]

 

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