祁连造山带玉石沟地幔橄榄岩中挥发分的流体化学和稳定同位素组成及古大洋岩石圈演化意义

胡沛青 张铭杰 汤中立 LI Chusi 王记周. 祁连造山带玉石沟地幔橄榄岩中挥发分的流体化学和稳定同位素组成及古大洋岩石圈演化意义[J]. 岩石学报, 2007, 23(1): 169-176.
引用本文: 胡沛青 张铭杰 汤中立 LI Chusi 王记周. 祁连造山带玉石沟地幔橄榄岩中挥发分的流体化学和稳定同位素组成及古大洋岩石圈演化意义[J]. 岩石学报, 2007, 23(1): 169-176.
HU PeiQing, ZHANG MingJie, TANG ZhongLi, LI ChuSi, WANG JiZhou , Lanzhou University, Lanzhou 730000, China; 2. Department of Geological Sciences, Indiana University, IN 47405, USA). Chemical and stable isotopic compositions of volatiles in mantle peridotites of the Yushigou ophiolite in Qilian orogenic belt, western China[J]. Acta Petrologica Sinica, 2007, 23(1): 169-176.
Citation: HU PeiQing, ZHANG MingJie, TANG ZhongLi, LI ChuSi, WANG JiZhou , Lanzhou University, Lanzhou 730000, China; 2. Department of Geological Sciences, Indiana University, IN 47405, USA). Chemical and stable isotopic compositions of volatiles in mantle peridotites of the Yushigou ophiolite in Qilian orogenic belt, western China[J]. Acta Petrologica Sinica, 2007, 23(1): 169-176.

祁连造山带玉石沟地幔橄榄岩中挥发分的流体化学和稳定同位素组成及古大洋岩石圈演化意义

  • 基金项目:

    This study was supported by grants from NSFC (40273009, 40534020), NCET and the State Key Lab of Gas-Geochemistry, Institute of Geology and Geophysics, CAS.

Chemical and stable isotopic compositions of volatiles in mantle peridotites of the Yushigou ophiolite in Qilian orogenic belt, western China

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出版历程
修回日期:  2006-07-15
刊出日期:  2007-01-31

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