黔东南地区新元古代下江群的地层年代及其地质意义

覃永军; 杜远生; 牟军; 卢定彪; 龙建喜; 王安华; 张厚松; 曾昌兴

doi:10.3799/dqkx.2015.093

Volume 40 Issue 7

Jul. 2015

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Article Navigation > Earth Science > 2015 > 40(7): 1107-1120

Qin Yongjun, Du Yuansheng, Mou Jun, Lu Dingbiao, Long Jianxi, Wang Anhua, Zhang Housong, Zeng Changxing, 2015. Geochronology of Neoproterozoic Xiajiang Group in Southeast Guizhou, South China, and Its Geological Implications. Earth Science, 40(7): 1107-1120. doi: 10.3799/dqkx.2015.093

Citation:

Qin Yongjun, Du Yuansheng, Mou Jun, Lu Dingbiao, Long Jianxi, Wang Anhua, Zhang Housong, Zeng Changxing, 2015. Geochronology of Neoproterozoic Xiajiang Group in Southeast Guizhou, South China, and Its Geological Implications. Earth Science, 40(7): 1107-1120. doi: 10.3799/dqkx.2015.093

Citation:

Qin Yongjun, Du Yuansheng, Mou Jun, Lu Dingbiao, Long Jianxi, Wang Anhua, Zhang Housong, Zeng Changxing, 2015. Geochronology of Neoproterozoic Xiajiang Group in Southeast Guizhou, South China, and Its Geological Implications. Earth Science, 40(7): 1107-1120. doi: 10.3799/dqkx.2015.093

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Geochronology of Neoproterozoic Xiajiang Group in Southeast Guizhou, South China, and Its Geological Implications

doi: 10.3799/dqkx.2015.093

Qin Yongjun^{1, 2, 3, 4
,},
Du Yuansheng^{1, 2
,
,},
Mou Jun⁴,
Lu Dingbiao⁴,
Long Jianxi⁴,
Wang Anhua⁴,
Zhang Housong⁴,
Zeng Changxing⁴

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.
Bureau of Geology and Mineral Exploration and Development of Guizhou Provience, Guiyang 550004, China
4.
Guizhou Geological Survey, Guiyang 550018, China

Received Date: 2014-12-12
Publish Date: 2015-07-15

Abstract

Abstract

Xiajiang Group in the Southeast Guizhou Province, as the western part of the Jiangnan orogen belt, consists of Precambrian low metamorphic terrisenous clastic sequence interlayer volcaniclastic rocks. But its age and stratigraphic correlation of the Precambrian are still controversial due to absence of lithologic marked bed and fossils and insufficient geochronological data. On the basis of detailed regional geology mapping of the sections, and zircon LA-ICP-MS geochronological study on tuff, tuffaceous and clastic rock of the Precambrian stratum in the study area, high resolution geological data to constrain the age of the Sibao and Xiajiang groups were obtained. It is found that the youngest weighted average ages of 819.8±6.4Ma from the clastic rock at the top of the Hechun Fm., Sibao Gp., for constraining the boundary age between the Sibao and Xiajiang groups. The Xiajiang Gp. can be divided into Wuye, Qingshuijiang, Pinglue and Longli formations from bottom to top. Tuffaceous clastic samples collected from each of the formation yield a series of age (779.5Ma, 764.0-756.0Ma, 733.9Ma and 725.0Ma) to represent the sedimentary times of these four formations. Based on these data, it is proposed that the depositional age of the Xiajiang and Sibao groups is limited to the Neoproterozoic. Combined with the field observation that the Longli and Chang'an formations are continuous deposits and the global low latitude glaciation event of Nanhuaian began from 717.4Ma, the sedimentary time of the Xiajiang Group can be constrained from 815Ma to 717Ma. Besides, the regional magmatic events further constrain the ages of the formations in the Xiajiang Group. The division and the stratigraphic correlation of the Xiajiang Group and the coeval strata help us to comprehend the evolution of the Xiajiang basin.
- stratigraphic age,
- zircon U-Pb age,
- Xiajiang Group,
- Precambrian,
- Jiangnan orogenic belt,
- geochronology

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Geochronology of Neoproterozoic Xiajiang Group in Southeast Guizhou, South China, and Its Geological Implications

doi: 10.3799/dqkx.2015.093

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