He and Ar isotopes in mantle megacryst minerals from Nushan and Yingfengling in Southeast China

被引:9
作者
Xu, SJ [1 ]
Fang, Z
Matsumoto, T
Matsuda, J
Yasuda, M
Yu, JH
Wang, RC
Liu, WZ
机构
[1] Osaka Univ, Dept Earth & Space Sci, Osaka 5600043, Japan
[2] Nanjing Univ, Dept Earth Sci, State Key Lab Mineral Deposits Res, Nanjing 210093, Peoples R China
来源
CHINESE SCIENCE BULLETIN | 2003年 / 48卷 / 15期
基金
中国国家自然科学基金;
关键词
mantle mineral; He and Ar isotope; depleted mantle; mantle contamination;
D O I
10.1360/02wd0506
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
He and Ar isotopic compositions of megacrystal minerals from mantle xenoliths were measured by the technique of vacuum crushing extraction. The used samples were clinopyroxene, garnet and ilmenite in Cenozoic alkaline basalts, which were from Nushan in Anhui Province and Ying-fengling in Guangdong Province, respectively, and represented materials from the upper mantle in the continental margin of SE China. The results show He-3/He-4 ratios of 7.99 Ra to 8.58 Ra, consistent with the characteristic ratios of the MORB-type mantle. 40Ar/39Ar ratios vary from 313 to 909, suggesting a binary mixing between the MORB-type mantle and air argons. This may reflect the incorporation of the air argon absorbed in oceanic sediments into the mantle beneath the continental margin by subduction of oceanic plate. This study presents the first report that ilmenite megacrysts contain abundant fluid inclusions and noble gases in the mantle xenoliths.
引用
收藏
页码:1624 / 1630
页数:7
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