扬子北缘大洪山地区中元古代打鼓石群碎屑锆石年代学及其地质意义

孔令耀; 毛新武; 陈超; 邓乾忠; 张汉金; 杨青雄; 李琳静; 李启文

doi:10.3799/dqkx.2017.039

Volume 42 Issue 4

Apr. 2017

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Article Navigation > Earth Science > 2017 > 42(4): 485-501

Kong Lingyao, Mao Xinwu, Chen Chao, Deng Qianzhong, Zhang Hanjin, Yang Qingxiong, Li Linjing, Li Qiwen, 2017. Chronological Study on Detrital Zircons and Its Geological Significance from Mesoproterozoic Dagushi Group in the Dahongshan Area, North Margin of the Yangtze Block. Earth Science, 42(4): 485-501. doi: 10.3799/dqkx.2017.039

Citation:

Kong Lingyao, Mao Xinwu, Chen Chao, Deng Qianzhong, Zhang Hanjin, Yang Qingxiong, Li Linjing, Li Qiwen, 2017. Chronological Study on Detrital Zircons and Its Geological Significance from Mesoproterozoic Dagushi Group in the Dahongshan Area, North Margin of the Yangtze Block. Earth Science, 42(4): 485-501. doi: 10.3799/dqkx.2017.039

Citation:

Kong Lingyao, Mao Xinwu, Chen Chao, Deng Qianzhong, Zhang Hanjin, Yang Qingxiong, Li Linjing, Li Qiwen, 2017. Chronological Study on Detrital Zircons and Its Geological Significance from Mesoproterozoic Dagushi Group in the Dahongshan Area, North Margin of the Yangtze Block. Earth Science, 42(4): 485-501. doi: 10.3799/dqkx.2017.039

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Chronological Study on Detrital Zircons and Its Geological Significance from Mesoproterozoic Dagushi Group in the Dahongshan Area, North Margin of the Yangtze Block

doi: 10.3799/dqkx.2017.039

Hubei Geological Survey, Wuhan430034, China

Received Date: 2016-09-18
Publish Date: 2017-04-15

Abstract

Abstract

There are many Pre-Nanhua strata and magmatic rocks in Yangtze Block, the detrital zircon preserved in sedimentary clastic rocks have great significances for limiting rock's age, tracing the source of sediments and revealing early evolution of the continent. This study is the first research of detrital zircon geochronology in both Lijiazui Formation and Luohanling Formation of Dagushi Group in the Dahongshan area, northern margin of the Yangtze block. The detrital zircons from Lijiazui Formation are dated a youngest age of 1 250±64 Ma, and several main age peaks of about 2 078 Ma, 2 437 Ma, 2 659 Ma and 3 084 Ma; the youngest age of Lijiazui Formation is 1 077±51 Ma, and it's ages peaks are about 1 126 Ma, 2 044 Ma, 2 458 Ma and 2 635 Ma. It is inferred that the sedimentary age of Lijiazui Formation is between 1 250±64 Ma and 1 126 Ma, and of Luohanling Formation is later than 1 077±51 Ma, indicating that Dagushi Group belongs to Mesoproterozoic. In addition, the age-histogram comparison of Dagushi Group and Shennongjia Goup, Kunyang Group, Dongchuan Group from different areas of Yangtze block, show that the source of these stratigraphic units are different from each other, which means the magmatic events and tectonic evolutions of each stratigraphic unit are different. Combined with previous research data of Yangtze block, we conclude that the blocks represented by each stratigraphic units are independent continent fragments in Mesoproterozoic, and amalgamated into the crystalline basement of the Yangtze block gradually in Mesoproterozoic to Neoproterozoic.
- Yangtze block,
- Mesoproterozoic,
- Dagushi Group,
- detrital zircon,
- geochronology

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References(106)

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Chronological Study on Detrital Zircons and Its Geological Significance from Mesoproterozoic Dagushi Group in the Dahongshan Area, North Margin of the Yangtze Block

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