SHRIMP age of the lava from the Sibao Group in Guilin and its chronostratigraphic significance

LI Li-yang; YOU Guo-qing; ZHANG Chuan-heng; JIA Long-long; HAN Yao; ZHANG Heng; LIU Bo; FENG Xin; LI Xin-fa; ZHANG Jin-long

doi:10.12029/gc20160610

2016 Vol. 43, No. 6

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Article navigation > Geology in China > 2016 > (6): 1992-1998

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LI Li-yang, YOU Guo-qing, ZHANG Chuan-heng, JIA Long-long, HAN Yao, ZHANG Heng, LIU Bo, FENG Xin, LI Xin-fa, ZHANG Jin-long. SHRIMP age of the lava from the Sibao Group in Guilin and its chronostratigraphic significance[J]. Geology in China, 2016, (6): 1992-1998. doi: 10.12029/gc20160610

Citation:

LI Li-yang, YOU Guo-qing, ZHANG Chuan-heng, JIA Long-long, HAN Yao, ZHANG Heng, LIU Bo, FENG Xin, LI Xin-fa, ZHANG Jin-long. SHRIMP age of the lava from the Sibao Group in Guilin and its chronostratigraphic significance[J]. Geology in China, 2016, (6): 1992-1998. doi: 10.12029/gc20160610

SHRIMP age of the lava from the Sibao Group in Guilin and its chronostratigraphic significance

1.
School of Earth Sciences and Resources, China University Of Geosciences(Beijing), Beijing 100083, China;No. 4 Gold Geological Party of CAPF, Liaoyang 111000, Liaoning, China
2.
Institute of Geology Chinese Academy of Geological Sciences, Beijing 100037, China
3.
School of Earth Sciences and Resources, China University Of Geosciences(Beijing), Beijing 100083, China
4.
No. 4 Gold Geological Party of CAPF, Liaoyang 111000, Liaoning, China

Received Date: 13 December 2015

Revised Date: 24 February 2016

Publish Date: 24 December 2016

Abstract

Abstract

The Sibao Group, outcropped in the north part of Guangxi and southeast part of Guizhou, is composed of over 5000 m thick succession of strongly-deformed, low-grade metamorphic volcanic rocks and terrigenous clastic rock, overlain unconformity by the Danzhou Group (Xiajiang Group). It is divided into three Formations:Jiuxiao Formation, Wentong Formation and Yuxi Formation. Sample A20140731-3 is lava, collected from the upper part of the Wentong Formation, and over 600 grains of zircon were sorted out from it. Fifteen of the zircons were analyzed with SHRIMP, and a weighed-mean U-Pb age of(860±13) Ma was obtained, which indicates that the volcanic rocks of the Sibao Group belong to Neoproterozoic. Based on this new zircon SHRIMP U-Pb age combined with the other high-quality ages obtained recently in the Jiangnan Orogen, the authors investigated the stratigraphic correlation between Sibao Group and the other main strata, such as Lengjiaxi Group, Shuangqiaoshan Group, and Fanjingshan Group.
- Sibao Group /
- zircon SHRIMP age /
- Neo-Proterozoic /
- Jiangnan Orogen