Meteorites from Mongolia

被引:10
作者
Bischoff, A
Gerel, O
Buchwald, VF
Spettel, B
Loeken, T
Schultz, L
Weber, HW
Schluter, J
Baljinnyam, L
Borchuluun, D
Byambaa, C
Garamjav, D
机构
[1] TECH UNIV, DEPT GEOL & MINERAL, ULAANBAATAR, MONGOLIA
[2] TECH UNIV DENMARK, DEPT MET, DK-2800 LYNGBY, DENMARK
[3] MAX PLANCK INST CHEM, D-55122 MAINZ, GERMANY
[4] UNIV HAMBURG, MINERAL MUSEUM, D-20146 HAMBURG, GERMANY
[5] STATE MUSEUM, MUSEUM NAT HIST, ULAANBAATAR, MONGOLIA
[6] MONGOLIAN ACAD SCI, ULAANBAATAR, MONGOLIA
[7] INST MINERAL RESOURCES, ULAANBAATAR, MONGOLIA
关键词
D O I
10.1111/j.1945-5100.1996.tb02063.x
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
The mineralogy and composition of six Mongolian meteorites were studied in some detail. Previously, only limited information existed about these rocks, and some were still unclassified. The six meteorites include three ordinary chondrites and three irons. The ordinary chondrite Adzhi-Bogdo (stone) is a regolith breccia (LL3-6) containing various types of clasts (some of foreign origin) embedded within a fine-grained elastic matrix. Tugalin Bulen (H6) and Noyan Bogdo (L6) meteorites are typical, well-metamorphosed ordinary chondrites. Adzhi-Bogdo (iron) has to be regarded as an IA iron meteorite like Campo del Cielo or Canyon Diablo; although the sample studied had been heated to about 900 degrees C-950 degrees C some time in the past, thus eradicating all original structural elements. Manlai is structurally closely related to the IIC iron meteorites; but based on its chemistry, which does not fit into this group, it is suggested that Manlai is an anomalous iron meteorite. The third iron, Sargiin Gobi, is certainly a normal member of the IA iron meteorites. The concentrations and isotopic compositions of He, Ne, and Ar were measured for all meteorites and their gas retention ages and exposure ages are discussed.
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页码:152 / 157
页数:6
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