ZIRCON U-PB CHRONOLOGY AND GEOCHEMICAL CHARACTERISTICS OF THE WUHEERTU GRANITE MASS IN LANGSHAN, INNER MONGOLIA

WANG Wen-long; TENG Xue-jian; LIU Yang; TENG Fei; GUO Shuo; HE Peng; TIAN Jian; DUAN Xiao-long

Volume 23 Issue 3

Jun. 2017

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Article Navigation > Journal of Geomechanics > 2017 > 23(3): 382-396

WANG Wen-long, TENG Xue-jian, LIU Yang, et al., 2017. ZIRCON U-PB CHRONOLOGY AND GEOCHEMICAL CHARACTERISTICS OF THE WUHEERTU GRANITE MASS IN LANGSHAN, INNER MONGOLIA. Journal of Geomechanics, 23 (3): 382-396.

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ZIRCON U-PB CHRONOLOGY AND GEOCHEMICAL CHARACTERISTICS OF THE WUHEERTU GRANITE MASS IN LANGSHAN, INNER MONGOLIA

Tianjin Center of Geological Survey, CGS, Tianjin 300170, China

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Received: 2016-09-24
Published: 2017-06-01

Abstract

Abstract

The WuheErtu granite mass, with the main rock types of syenogranite and monzogranite, are distributed in Langshan area, Inner Mongolia, northern margin of the North China Plate. Zircon U-Pb ageis 236.1±1.0Ma, indicating the WuherErtu granite mass formed in late Triassic.Geochemical results show high content of SiO₂(71.94~73.91%), K₂O+Na₂O(8.34~8.88%), low content of Ca and Mg, and weak content of aluminum(0.98 < A/CNK < 1.07). In SiO₂-K₂O diagram, sample points fall into the transitional region between high-K calc-alkaline and Shoshonite series. In the primitive mantle-normalized spider diagram, the geochemical characteristics of the granite mass show in some degree enrichment in Rb、Th、K、Nd、Zr、Hf、Sm and depletion in Ba、Nb、Ta、Sr、P、Ti, with medium to negligible Eu anomalies (δEu=0.47~0.66), which indicate the WuherErtu granite mass belong to the post-collisional granite formed in the tectonic setting transformed from compression system to extension system. Zircon Hf isotopic displays that εHf(t) values vary from -20.6 to +7.6 and Hf model ages (TDM2) vary from 780~2559 Ma, which suggest a mixed magma source of old continental crust with a small involvement of juvenile components.The comprehensive study of this granite mass helps to further understand and explore the tectonic-magmatic evolution of the northern margin of the North China plate in late Permian-Triassic.
- Inner Mongolia,
- Langshan area,
- the triassic granite,
- post-collision,
- geochemistry

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References(71)

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