西藏班公湖-怒江缝合带中段江错蛇绿岩岩石学、地球化学、年代学及地质意义

黄强太; 李建峰; 夏斌; 殷征欣; 郑浩; 石晓龙; 胡西冲

doi:10.3799/dqkx.2015.003

Volume 40 Issue 1

Jan. 2015

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Huang Qiangtai, Li Jianfeng, Xia Bin, Yin Zhengxin, Zheng Hao, Shi Xiaolong, Hu Xichong, 2015. Petrology, Geochemistry, Chronology and Geological Significance of Jiang Tso Ophiolite in Middle Segment of Bangonghu-Nujiang Suture Zone, Tibet. Earth Science, 40(1): 34-48. doi: 10.3799/dqkx.2015.003

Citation:

Huang Qiangtai, Li Jianfeng, Xia Bin, Yin Zhengxin, Zheng Hao, Shi Xiaolong, Hu Xichong, 2015. Petrology, Geochemistry, Chronology and Geological Significance of Jiang Tso Ophiolite in Middle Segment of Bangonghu-Nujiang Suture Zone, Tibet. Earth Science, 40(1): 34-48. doi: 10.3799/dqkx.2015.003

Citation:

Huang Qiangtai, Li Jianfeng, Xia Bin, Yin Zhengxin, Zheng Hao, Shi Xiaolong, Hu Xichong, 2015. Petrology, Geochemistry, Chronology and Geological Significance of Jiang Tso Ophiolite in Middle Segment of Bangonghu-Nujiang Suture Zone, Tibet. Earth Science, 40(1): 34-48. doi: 10.3799/dqkx.2015.003

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Petrology, Geochemistry, Chronology and Geological Significance of Jiang Tso Ophiolite in Middle Segment of Bangonghu-Nujiang Suture Zone, Tibet

doi: 10.3799/dqkx.2015.003

Huang Qiangtai^{1, 2, 3
,},
Li Jianfeng⁴,
Xia Bin^{1, 2, 3
,
,},
Yin Zhengxin^{1, 2, 3},
Zheng Hao^{1, 2, 3},
Shi Xiaolong^{1, 2, 3},
Hu Xichong^{1, 2, 3}

1.
School of Marine Sciences, Sun Yat-Sen University, Guangzhou 510006, China
2.
Key Laboratory of Offshore Oil Exploration and Development, Guangdong Universities, Guangzhou 510006, China
3.
Guangdong Provincial Key Laboratory of Marine Resources and Coastal Engineering, Guangzhou 510006, China
4.
Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China

Received Date: 2014-05-25
Publish Date: 2015-01-15

Abstract

Abstract

Jiang Tso ophiolite, which belongs to the most eastern part of Qieli Lake ophiolite subzone, is located at the middle segment of the Bangonghu-Nujiang suture zone to the south of Pung Lake ophiolite. The rock association of Jiang Tso ophiolite is relatively complete and mainly composed of metamorphic peridotite, gabbro and diabase. Comparing with N-MORB, the major and trace elements of Jiang Tso ophiolite are characterized with high content in Mg and low contents in Ti, K, Na, P and the depletion of elements of Nb, Ta, Hf, and Th. In addition, it displays relative enrichment of Rb, Sr, and Ba. Geochemistry characteristics of the Jiang Tso ophiolite indicate it is of supra-subduction zone type ophiolite and formed in the spreading ridge of back arc basin. The zircon SHRIMP U-Pb weighted average ages of gabbro is 189.8±3.3 Ma (MSWD=0.97), which suggests that the extension time of Tethys oceanic basin in Jiang Tso region was consistent with the formation time of the Dongqiao oceanic basin in the middle part, and also corresponding to that of the oceanic basin in the western part, while later than the development of oceanic basin in the eastern part of the Bangonghu-Nujiang suture zone. From the geochronological data, it can be deduced that the development of the Bangonghu-Nujiang oceanic basin was characterized by being gradually later from east to west.
- Jiang Tso ophiolite,
- geochemistry,
- SHRIMP U-Pb dating,
- tectonic environment,
- Tibet

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References(105)

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Petrology, Geochemistry, Chronology and Geological Significance of Jiang Tso Ophiolite in Middle Segment of Bangonghu-Nujiang Suture Zone, Tibet

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