滇东南八布早二叠世含火山岩屑砂岩指示古特提斯洋俯冲

杨江海; 杜远生; 于鑫; 黄虎; 柴嵘

doi:10.3799/dqkx.2017.002

Volume 42 Issue 1

Jan. 2017

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Yang Jianghai, Du Yuansheng, Yu Xin, Huang Hu, Chai Rong, 2017. Early Permian Volcanic Fragment-Bearing Sandstones in Babu of SoutheastYunnan: Indicative of Paleo-Tethyan Ocean Subduction. Earth Science, 42(1): 24-34. doi: 10.3799/dqkx.2017.002

Citation:

Yang Jianghai, Du Yuansheng, Yu Xin, Huang Hu, Chai Rong, 2017. Early Permian Volcanic Fragment-Bearing Sandstones in Babu of SoutheastYunnan: Indicative of Paleo-Tethyan Ocean Subduction. Earth Science, 42(1): 24-34. doi: 10.3799/dqkx.2017.002

Citation:

Yang Jianghai, Du Yuansheng, Yu Xin, Huang Hu, Chai Rong, 2017. Early Permian Volcanic Fragment-Bearing Sandstones in Babu of SoutheastYunnan: Indicative of Paleo-Tethyan Ocean Subduction. Earth Science, 42(1): 24-34. doi: 10.3799/dqkx.2017.002

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Early Permian Volcanic Fragment-Bearing Sandstones in Babu of SoutheastYunnan: Indicative of Paleo-Tethyan Ocean Subduction

doi: 10.3799/dqkx.2017.002

Yang Jianghai^{1,2
,},
Du Yuansheng^1,2,
Yu Xin^1,2,
Huang Hu³,
Chai Rong^1,2

1.
State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan 430074, China
2.
School of Earth Sciences, China University of Geosciences, Wuhan 430074, China
3.
Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu 610059, China

Received Date: 2016-08-10
Publish Date: 2017-01-15

Abstract

Abstract

Babu mafic/ultramafic rocks in Southeast Yunnan Province are interpreted as remnant ocean crust, and together with the ophiolite in Song Hien tectonic zone of North Vietnam, constitute significant components of the Babu-Song Hien Paleo-Tethyan suture, a possible southern extension of the Ailaoshan suture. Around the Babu ophiolite is a widespread siliclastic rocks dominated sequence, with thin-bedded cherts observed in some locations. These clastic rocks have long been considered to be Triassic turbidity current deposits in spite of absence of reliable fossil and isotopic dating. West to Longlin village, there outcrop coarse sandstone and sandy conglomerate beds nearby the Babu mafic/lutramific rocks. These sandstones contain andesite and rhyolite fragments and display detrital zircon age spectra similar to those of the Late Permian sandstones in Song Hien tectonic zone and Permian sandstones in western Ailaoshan belt, but distinguished from those of the Permian-Triassic clastic rocks of Youjiang and Shiwandashan basins in southwestern South China. The youngest zircon group with ages of ~285Ma, has geochemical affinities of magmatic zircons crystallized from arc/orogenic settings, corresponding to the occurrence of volcanic rock fragments, indicating a maximum depositional age, and showing an adjacent Early Permian volcanic source. The new findings of chert deposits within a clastic rock section to the east of Babu Village, and the comparison of detrital zircon U-Pb age spectra suggest that the analyzed clastic rocks should be Early Permian rather than Middle Triassic in age and their Permian volcanic source might be related to the subduction of Babu-Song Hien Paleo-Tethyan ocean.
- Babu clastic rock,
- Early Permian,
- Paleo-Tethyan ocean subduction,
- detrital zircon,
- volcanic rock fragment,
- petrology

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References(84)

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Early Permian Volcanic Fragment-Bearing Sandstones in Babu of SoutheastYunnan: Indicative of Paleo-Tethyan Ocean Subduction

doi: 10.3799/dqkx.2017.002

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