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U-Pb Dating of Detrital Zircon from Lower Silurian in Keping Area of Tarim Basin and Its Geological Implication(PDF)

《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

Issue:
2012年第03期
Page:
32-43
Research Field:
基础地质与矿产地质
Publishing date:

Info

Title:
U-Pb Dating of Detrital Zircon from Lower Silurian in Keping Area of Tarim Basin and Its Geological Implication
Author(s):
CHANG Jian12 QIU Nan-sheng12 LI Jia-wei12
1. State Key Laboratory of Petroleum Resource and Prospecting, China University of Petroleum, Beijing 102249,China; 2. Basin and Reservoir Research Center, China University of Petroleum, Beijing 102249, China
Keywords:
detrital zircon U-Pb dating Silurian provenance Shaya Uplift Tazhong Uplift Keping Area Tarim Basin
PACS:
P597.3
DOI:
-
Abstract:
The provenance and evolution in Keping Area are closely correlated with the paleogeography of Tarim Basin. The morphology of detrital zircon and distribution characteristics of U-Pb age in Lower Silurian were analyzed, and the provenance and evolution from Lower Silurian in Keping Area were systematically studied. The results showed that the zircons from Lower Silurian in Keping Area were magmatic, zircon U-Pb age represented diagenesis age or crystallinic age and effectively indicated the provenance; the provenances in Kalpintag Formation of Lower Silurian were mainly western Shaya Uplift, Tazhong Uplift and the frontal uplift in the southwestern of Tarim Basin, and then Tazhong Uplift was covered by seawater due to the transgression, the provenances in Tataaiertag Formation of Lower Silurian became the western Shaya Uplift, the frontal uplift in the southwestern of Tarim Basin and the Yutian and Kangxiwa Areas in the southern of Tazhong Uplift; the provenance in Keping Area was different with that in the central and eastern of Tarim Basin because of Manjiaer Sag; the zircon ages of 900-700 Ma illustrated that Tarim Block was related to Gondwanaland.

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Last Update: 2012-09-20