黔东震旦-寒武系转换期碎屑锆石年龄及其地质意义

杨恩林; 吕新彪; 石平; 吴波; 刘文; 狄永宁

doi:10.3799/dqkx.2014.037

Volume 39 Issue 4

Apr. 2014

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Article Navigation > Earth Science > 2014 > 39(4): 387-398

Yang Enlin, Lü Xinbiao, Shi Ping, Wu Bo, Liu Wen, Di Yongning, 2014. Detrital Zircon Age of Stratigraphic Sinian-Cambrian in East Guizhou and Its Geological Significance. Earth Science, 39(4): 387-398. doi: 10.3799/dqkx.2014.037

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Yang Enlin, Lü Xinbiao, Shi Ping, Wu Bo, Liu Wen, Di Yongning, 2014. Detrital Zircon Age of Stratigraphic Sinian-Cambrian in East Guizhou and Its Geological Significance. Earth Science, 39(4): 387-398. doi: 10.3799/dqkx.2014.037

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Detrital Zircon Age of Stratigraphic Sinian-Cambrian in East Guizhou and Its Geological Significance

doi: 10.3799/dqkx.2014.037

Yang Enlin^{1, 2
,},
Lü Xinbiao^{1
,
,},
Shi Ping²,
Wu Bo²,
Liu Wen³,
Di Yongning⁴

1.
Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, China
2.
117 Geological Team, Bureau of Geology and Mineral Exploration and Development of Guizhou Province, Guiyang 550018, China
3.
Geological Survey, China University of Geosciences, Wuhan 430074, China
4.
School of Geographic and Environmental Sciences, Guizhou Normal University, Guiyang 550001, China

Received Date: 2013-07-19
Publish Date: 2014-04-15

Abstract

Abstract

Lithology, ore-bearing potential and contact relation in Zhuxi stratigraphic section are studied in detail. 84 groups of effective ages concentrated in 864-742 Ma are obtained from U-Pb dating of detrital zircon by LA-ICP-MS in feldspar lithic sandstone in the black shales, which indicates the presence of large-scale magmatic activity of the East Guizhou at the Neoproterozoic. All zircon U-Pb ages indicate that sediments within Lower Cambrian black shales in East Guizhou are mainly from the Jiangnan orogen. Metal elements such as vanadium are derived from the basic-ultrabasic rocks. The Xuefeng movement peeled the top of ore-bearing rock off the basic-ultrabasic rocks, pouring a great amount of metal into the ocean. The anoxic submarine caused the death of algae whose bodies were rich of metallogenic elements, which introduced vanadium into the sediments along with the organic matter. The mineralization occurred in the Liuchapo and Jiumenchong formations that were favorable to sedimentation of metals. 536 Ma is the final depositional time of the Jiumenchong Formation, and maximum depositional age of the Liuchapo Formation. The boundary between Sinian and Cambrian is located in the upper siliceous rocks of the Liuchapo Formation. Lithology deformation, metamorphism, and unconformity with other strata of the Qingshuijiang Formation are the geological responses of the Xuefeng movement.
- stratigraphy,
- detrital zircon,
- sedimentology,
- geochronology,
- Zhuxi section

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References(76)

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