LA-ICP-MS zircon U-Pb dating and tectonic setting of the monzogranites in the Fengleishan area of Beishan orogenic belt, Inner Mongolia

HAO Zengyuan; GAO Jian; WANG Chen; LIU Xudong; LI Decheng; WANG Xinliang

doi:10.12029/gc20200419

GEOLOGY IN CHINA > 2020 > 47(4): 1204-1219. > DOI: 10.12029/gc20200419

HAO Zengyuan, GAO Jian, WANG Chen, LIU Xudong, LI Decheng, WANG Xinliang. LA-ICP-MS zircon U-Pb dating and tectonic setting of the monzogranites in the Fengleishan area of Beishan orogenic belt, Inner Mongolia[J]. GEOLOGY IN CHINA, 2020, 47(4): 1204-1219. DOI: 10.12029/gc20200419

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LA-ICP-MS zircon U-Pb dating and tectonic setting of the monzogranites in the Fengleishan area of Beishan orogenic belt, Inner Mongolia

1.
Xi'an Institute of Geological Survey and Mineral Exploration, Xi'an 710100, Shaanxi, China
2.
Inner Mongolia Institute of Geological Survey and Mineral Exploration, Hohhot 010010, Inner Mongolia, China
3.
Shaanxi Bureau of Geology and Mineral Resources, Xi'an 710100, Shaanxi, China

Funds:

the project of China Geological Survey 1212011220462

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Author Bio:
HAO Zengyuan, male, born in 1987, engineer, engages in regional and mineral geological survey; E-mail:714044937@qq.com
Received Date: November 14, 2018
Revised Date: December 02, 2019
Available Online: September 25, 2023

Graphical Abstract

Abstract

Abstract

Monzogranites in Fengleishan are located in northern Beishan and situated between two ophiolitic mélange belts of Hongshishan-Baiheshan-Pengboshan and Jijitaizi-Xiaohuangshan, having a special tectonic affinity. Zircons from the monzogranites yielded a weighted mean LA-ICP-MS U-Pb age of (320±1) Ma, representing the intrusion age. The samples are characterized by high content of SiO₂ and Al₂O₃ with Rittmann indexes of 1.58-2.74 (< 3.3) and alkaline ratios of 2.35-4.05, belonging to calc-alkaline granitoids. Their A/NCK values range from 0.92 to 1.15 and display metaaluminous to peraalmuinous affinities. They have relatively high content of total REE and are characterized by LREE-enriched patterns ((La/Yb)_N=4.60-8.83)and negative Eu anomalies (δEu=0.56-0.88, 0.72 in average). They also show strong enrichment of incompatible elements (e.g., Th and U) and large ion lithophile elements (e.g., Rb and K) but depletion of high field strength elements (e.g., Nb, Ta, Ti and P). Their normalized patterns are similar to those of upper continental crust (UPC), indicating participation of materials from the UPC in their magma source. High values of Th (8.58-21.62 μg/g) and low ratios of Nb/Ta (8.75-15.72) point to a crust-dominated magma source. On the tectonic discriminant diagrams of Rb-(Nb+Y) and R₁-R₂, most of the samples are plotted in the pre-collisional volcanic arc granite area. Based on associated lithological characteristics, it is proposed that monzogranites in the Fengleishan were formed by pre-collisional volcanic arc magmatism, which was related to oceanic crust subduction in the Hongshishan-Baiheshan-Pengboshan belt. Combined with regional geological background, it is inferred that the closure of the small ocean in the Hongshishan-Baiheshan-Pengboshan belt should postdate the early period of late Carboniferous.
- Beishan orogenic belt,
- zircon U-Pb age,
- geochemistry,
- active continental margin,
- geological survey engineering,
- Fengleishan,
- Inner Mongolia

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References (150)

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LA-ICP-MS zircon U-Pb dating and tectonic setting of the monzogranites in the Fengleishan area of Beishan orogenic belt, Inner Mongolia