大兴安岭早白垩世伸展作用: 内蒙古乌拉盖球状岩地球化学及锆石U-Pb定年的限制

汪岩; 钱程; 庞雪娇; 马永非; 张立东; 杨雅军; 钟辉

doi:10.3799/dqkx.2020.165

Volume 46 Issue 4

Apr. 2021

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Article Navigation > Earth Science > 2021 > 46(4): 1447-1466

Wang Yan, Qian Cheng, Pang Xuejiao, Ma Yongfei, Zhang Lidong, Yang Yajun, Zhong Hui, 2021. Early Cretaceous Extension of Great Xing'an Range: Constraints from Geochemistry and Zircon U-Pb Ages of Orbicular Rocks in Uragai Area, Inner Mongolia, China. Earth Science, 46(4): 1447-1466. doi: 10.3799/dqkx.2020.165

Citation:

Wang Yan, Qian Cheng, Pang Xuejiao, Ma Yongfei, Zhang Lidong, Yang Yajun, Zhong Hui, 2021. Early Cretaceous Extension of Great Xing'an Range: Constraints from Geochemistry and Zircon U-Pb Ages of Orbicular Rocks in Uragai Area, Inner Mongolia, China. Earth Science, 46(4): 1447-1466. doi: 10.3799/dqkx.2020.165

Citation:

Wang Yan, Qian Cheng, Pang Xuejiao, Ma Yongfei, Zhang Lidong, Yang Yajun, Zhong Hui, 2021. Early Cretaceous Extension of Great Xing'an Range: Constraints from Geochemistry and Zircon U-Pb Ages of Orbicular Rocks in Uragai Area, Inner Mongolia, China. Earth Science, 46(4): 1447-1466. doi: 10.3799/dqkx.2020.165

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Early Cretaceous Extension of Great Xing'an Range: Constraints from Geochemistry and Zircon U-Pb Ages of Orbicular Rocks in Uragai Area, Inner Mongolia, China

doi: 10.3799/dqkx.2020.165

Shenyang Center of China Geological Survey, Shenyang 110034, China

Received Date: 2020-03-13
Publish Date: 2021-04-15

Abstract

Abstract

In addition to its beautiful structure, the newly discovered orbicular rocks in the central and southern parts of the Great Xing'an volcanic belt in the Uragai region are of great importance to the exploration of the subduction history of the Great Xing'an Range in the NE China. On the basis of detailed field geological survey, in this paper it makes a comprehensive study on the geochemistry and Sr-Nd isotope characteristics of the orbicular rocks and its host rocks in Uragai area, Inner Mongolia, and discusses its magmatic source and formation mechanism. The analysis results show that the Uragai orbicular rock and its host rocks have high silica (SiO₂=75.35%-76.21%) and alkali (K₂O+Na₂O=7.30%-7.45%), but low aluminium (Al₂O₃=9.82%-11.30%), Mg^# value (Mg^#=4.52-14.47), chromium (Cr=14.5×10^-6-22.5×10^-6), and nickel (Ni=1.84×10^-6-3.97×10^-6), indicating a crustal magmatic source. Trace and rare earth elements (REEs) show post-orogenic volcanic rock features: obviously enriched in large ion lithophile elements (LILEs, e.g., Rb, Th, K, LREE) and high field strength elements (HFSEs, e.g., Nb, Ta, Zr, HREE). The Nb negative anomaly is not obvious in N-MORB standardized diagram, with significant differentiation between light rare earth elements (LREE) and heavy rare earth elements (HREE) (LREE/HREE=5.21-6.70). The initial ⁸⁷Sr/⁸⁶Sr (0.705 9-0.713 7) is higher than the MORB of modern ocean (0.702 29-0.703 34), which also suggests a crustal source. However, the ¹⁴³Nd/¹⁴⁴Nd (0.512 456-0.512 528) was lower than the value of modern oceans (0.512 99-0.513 30), and with ε_Nd value from +4.8 to +6.2, which shows depleted mantle signature. Study shows that the magmatic source of Uragai orbicular rock and its host rocks originated from the lower crust, and with participation of depleted mantle material. The obviously depleted Sr, Ba and Eu suggest the fractional crystallization course, and the rocks formed in a stable in-plate tectonic environment. Major and trace element diagrams also show the post-orogenic A-type granite features. The study shows that the orbicular rocks have few reliable geological ages, probably resulted from sufficient low temperature fluids which blocked the crystallization course. The abundant trapped zircons or other refractory minerals may provide a material basis for the formation of orbicular rocks. The zircon LA-ICP-MS U-Pb age of graphic granite in the main face of the orbicular rocks is 142.2±2.7 Ma, and the average age of diabase dikes in the orbicular rocks is 140.5 Ma, and the zircon LA-ICP-MS U-Pb age obtained from orthophyre, which is surrounding rocks of the main face of the orbicular rocks, is 349.5±3.4 Ma, These age information restricted the formation age of orbicular rocks at Early Cretaceous(141 Ma±), its host rocks is Early Carboniferous, which is totally different with host rocks of orbicular rocks in and abroad. Comprehensive research shows that the formation mechanism of orbicular rock and its host rocks in Uragai area is related to late stage magmatic activity in the Great Xing'an volcanic belt, largely controlled by the post-orogenic extension tectonic setting of the Mongol-Okhotsk Ocean in the Early Cretaceous, and it is a product of the large-scale regional extension and strong magmatic underplating in the Great Xing'an Range.
- orbicular rock,
- isotope chronology,
- geochemistry,
- regional extension,
- Great Xing'an Range,
- Uragai area,
- Inner Mongolia

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Early Cretaceous Extension of Great Xing'an Range: Constraints from Geochemistry and Zircon U-Pb Ages of Orbicular Rocks in Uragai Area, Inner Mongolia, China

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