晚三叠世金沙江结合带碰撞作用：贡觉石英二长岩年代学、地球化学及Hf同位素证据

巩小栋; 唐渊; 秦雅东; 王保弟; 王冬兵; 刘函; 段瑶瑶

doi:10.3799/dqkx.2020.221

Volume 45 Issue 8

Aug. 2020

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Gong Xiaodong, Tang Yuan, Qin Yadong, Wang Baodi, Wang Dongbing, Liu Han, Duan Yaoyao, 2020. Late Triassic Collision of Jinshajiang Suture Belt: Geochronological, Geochemical and Hf Isotope Evidences from Quartz Monzonite in Gonjo Area. Earth Science, 45(8): 2905-2919. doi: 10.3799/dqkx.2020.221

Citation:

Gong Xiaodong, Tang Yuan, Qin Yadong, Wang Baodi, Wang Dongbing, Liu Han, Duan Yaoyao, 2020. Late Triassic Collision of Jinshajiang Suture Belt: Geochronological, Geochemical and Hf Isotope Evidences from Quartz Monzonite in Gonjo Area. Earth Science, 45(8): 2905-2919. doi: 10.3799/dqkx.2020.221

Citation:

Gong Xiaodong, Tang Yuan, Qin Yadong, Wang Baodi, Wang Dongbing, Liu Han, Duan Yaoyao, 2020. Late Triassic Collision of Jinshajiang Suture Belt: Geochronological, Geochemical and Hf Isotope Evidences from Quartz Monzonite in Gonjo Area. Earth Science, 45(8): 2905-2919. doi: 10.3799/dqkx.2020.221

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Late Triassic Collision of Jinshajiang Suture Belt: Geochronological, Geochemical and Hf Isotope Evidences from Quartz Monzonite in Gonjo Area

doi: 10.3799/dqkx.2020.221

Chengdu Center of China Geological Survey, Chengdu 610081, China

Received Date: 2020-03-19
Publish Date: 2020-08-15

Abstract

Abstract

As one of the important suture belts in the Sanjiang Tethyan tectonic domain, the Jinshajiang suture belt has long been the focus of study on the process of Paleo-Tethys ocean-continent subduction and collision. However, controversies remain about the exact time for the collision and closure of the Jinshajiang Paleo-Tethys. In this paper, the Gonjo granite body was selected as the research object, which is located on the west side of the Jinshajiang suture belt in the eastern Tibet. Based on the chronological, geochemical and Hf isotope analyses of the large-scale exposed quartz monzonite, the geochemical characteristics and tectonic setting of the Gonjo granite body are revealed. LA-ICP-MS zircon U-Pb dating results yield a weighted mean ²⁰⁶Pb/²³⁸U age of 231±1 Ma for the sample, indicating that quartz monzonite was emplaced in Late Triassic. Zircon from the quartz monzonite exhibits a narrow range of initial Hf isotope ratios (ε_Hf(t)=-8.3 to -5.5), with corresponding T_DMC of 1 611-1 788 Ma.Geochemical studies show that the quartz monzonite is typical I-type granite, belonging to shoshonite and high K calc-alkali series, enriched in Rb, Th, K, and LILEs, but depleted in Nb, Ta, Zr, Hf and HFSEs. In addition, geochemical features show that the quartz monzonite was formed in the geological background of continent collision, suggesting that the Gonjo area was in a transition phase of syn-collision compressional to post-collisional extension stage in the Early Triassic (~231 Ma) and the quartz monzonite was a product of partial melting of lower crustal intermediate-basic igneous rocks. Combined with previous studies, it can be proposed that the Paleo-Tethys ocean of Jinshajiang suture was gradually closed from south to north, and the differences of regional geological background and the complexity of the Paleo-Tethys ocean oblique collision are the main reasons for the different collision-closure time of different regions of the Jinshajiang suture belt.
- Jinshajiang suture belt,
- quartz monzonite,
- zircon U-Pb dating,
- Hf isotope,
- Late Triassic,
- Paleo-Tethys

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References(104)

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