西藏玛日埃错地区花岗斑岩岩石成因及其对班公湖-怒江缝合带中段演化的制约

李发桥; 刘治博; 唐菊兴; 宋扬; 高轲; 李海峰; 赵志强; 滕磊

doi:10.3799/dqkx.2018.709

Volume 43 Issue 4

Apr. 2018

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Li Faqiao, Liu Zhibo, Tang Juxing, Song Yang, Gao Ke, Li Haifeng, Zhao Zhiqiang, Teng Lei, 2018. Petrogenesis of Granite Porphyry in Mariaicuo Area, Shuanghu County, Tibet, and Constraints on the Evolution in the Middle Section of Bangonghu-Nujiang Suture Zone. Earth Science, 43(4): 1051-1069. doi: 10.3799/dqkx.2018.709

Citation:

Li Faqiao, Liu Zhibo, Tang Juxing, Song Yang, Gao Ke, Li Haifeng, Zhao Zhiqiang, Teng Lei, 2018. Petrogenesis of Granite Porphyry in Mariaicuo Area, Shuanghu County, Tibet, and Constraints on the Evolution in the Middle Section of Bangonghu-Nujiang Suture Zone. Earth Science, 43(4): 1051-1069. doi: 10.3799/dqkx.2018.709

Citation:

Li Faqiao, Liu Zhibo, Tang Juxing, Song Yang, Gao Ke, Li Haifeng, Zhao Zhiqiang, Teng Lei, 2018. Petrogenesis of Granite Porphyry in Mariaicuo Area, Shuanghu County, Tibet, and Constraints on the Evolution in the Middle Section of Bangonghu-Nujiang Suture Zone. Earth Science, 43(4): 1051-1069. doi: 10.3799/dqkx.2018.709

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Petrogenesis of Granite Porphyry in Mariaicuo Area, Shuanghu County, Tibet, and Constraints on the Evolution in the Middle Section of Bangonghu-Nujiang Suture Zone

doi: 10.3799/dqkx.2018.709

Li Faqiao^{1,2
,},
Liu Zhibo^{2
,
,},
Tang Juxing²,
Song Yang²,
Gao Ke³,
Li Haifeng^1,2,
Zhao Zhiqiang¹,
Teng Lei^1,2

1.
School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China
2.
Key Laboratory of Metallogeny and Mineral Assessment of Ministry of Land and Resources, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China
3.
School of Earth Sciences, Chengdu University of Technology, Chengdu 610059, China

Received Date: 2017-12-20
Publish Date: 2018-04-15

Abstract

Abstract

LA-ICP-MS zircon U-Pb dating, geochemical and Sr-Nd-Pb isotopic data analysis were conducted on the granite porphyry in Mariaicuo area in order to determine its formation time, petrogenesis, structural setting and geological significance. LA-ICP-MS zircon U-Pb dating of the granite porphyry in Mariaicuo yields a crystallization age of 78.3±0.4 Ma, indicating that the rock formed in the late of Late Cretaceous. Petrogeochemically, the samples of the rocks are high in SiO₂ (72.41%-74.06%) and rich in Na₂O+K₂O of 6.66%-7.14%, which belong to calc-alkaline series. Its A/CNK ratios of 1.01-1.07 are of characteristics of weakly peraluminous granites. They are enriched in the large-ion lithospile elements of Rb, Ba, U, K and Th, and strongly depleted in high field strength elements Nb, Ta, P, and Ti. The REE distribution mode is obvious right-leaning, indicating that it remains garnet-amphibolite facies in source area. Their isotopic compositions are characterized by low initial (⁸⁷Sr/⁸⁶Sr)_i of 0.705 2-0.706 0 and low positive ε_Nd(t) (1.5-2.3) values and relatively young second-stage model age (t_DM2=692-758 Ma) of crust. It has relatively homogeneous Pb isotope composition with the evolution of orogenic characteristics. Comprehensive analysis shows that the granite porphyry in Mariaicuo area may originate from the new partial melting of crust within extensional background, and its source region is enriched in fluid and remains garnet-amphibolite facies, excluding plagioclase. It formed in the post-collision extensional environment, which occurred after the closure of Bangonghu-Nujiang Tethys Ocean (BTO) and collision between tarranes on both sides, when the middle section of Bangonghu-Nujiang suture zone has entered the extension phase in Late Cretaceous.
- petrogenesis,
- post-collision,
- granite porphyry,
- Mariaicuo area,
- middle section of Bangonghu-Nujiang suture zone,
- petrology

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References(148)

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