Journal of Jilin University(Earth Science Edition) ›› 2021, Vol. 51 ›› Issue (3): 767-782.doi: 10.13278/j.cnki.jjuese.20200183

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Petro-Geochemical Characteristics and Geological Significance of Dishantou Granite Body in East Kunlun Orogenic Belt

Deng Hongbin, Li Peilong, Wei Huacai, He Wenjin, Yang Pengtao, Li Ning, Tang Hua   

  1. Sichuan Northwest Geological Team, Bureau of Exploration and Exploitation of Geology and Mineral Resources of Sichuan Province, Mianyang 621000, Sichuan, China
  • Received:2020-08-11 Online:2021-05-26 Published:2021-06-07
  • Supported by:
    Supported by the Project of China Geological Survey (12120114000201) and the Geological Exploration Fund Project of Qinghai Provincial Department of Natural Resources (Qingdidiaokan[2017]No.247)

Abstract: The granite body in Dishantou area belongs to the North Kunlun magmatic arc belt of the East Kunlun arc basin. It is located in the middle part of the East Kunlun orogenic belt in the Berkarik Xiangride metallogenic sub belt of the East Kunlun metallogenic belt. The main rock types are quartz diorite, syenogranite and monzogranite. To strengthen the study on the petro-geochemistry and diagenesis and metallogenic background of the granitic bodies in this area, the analysis on the major elements, trace elements, and mineral elements of the granitic bodies has been carried out. The quartz diorite has the characteristics of medium silicon (57.64% and 58.47%) and rich sodium (Na2O/K2O is 2.57) in the composition of the main elements. The syenogranite is characterized by high silicon (75.45%-75.99%) and rich potassium (Na2O/K2O is 0.74-0.94). The monzogranite is characterized by high silicon (66.80%-73.45%) and rich sodium (Na2O/K2O is 1.50-2.13). A/CNK of the granitic body is less than 1, indicating that it is aluminous magmatic rock. The alkali saturation index (NK/A) ranges from 0.26 to 0.69, belonging to calc-alkaline type. The light rare earth elements are relatively enriched in heavy rare earth elements (characteristics of magmatic differentiation), large ion lithophile elements (LILE) of Rb, K, Ba, Th, Sr and Nd, only syenogranite is depleted in Sr; Meanwhile, high field strength elements (HFSE) are rich in Zr, Hf and Ce, but Nb, P, and Ti are depleted apparently, indicating the source materials of crust-mantle mixing, formed under an extrusion stress environment with collision type I granite. In 11 kinds of elements analysis of data obtained from the rock mass, compared with the average element abundances of Qinghai Province, the East Kunlun metallogenic belt and its sub metallogenic belt, the granite types with different lithology and different ages are preliminarily divided, and the enriched ore-bearing elements are Au, Zn, Y, Pb, etc. Compared with the regional metallogenic facts and the genesis of I-type granites, the study area has a good prospecting potential.

Key words: petrogenesis, granite body, geochemistry, mineral elements, East Kunlun orogenic belt, Dishantou area

CLC Number: 

  • P581
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[2] LI Xian-zhou,LIU Yan,LIU Li-hua,NING Wei-kun,FAN Hai. The Preparation and Characterization of the Kaolin-Hydrazine Intercalation Complex[J]. J4, 2006, 36(04): 659 -662 .
[3] LU Shuang-fang, LI Ji-jun, XUE Hai-tao, XU Li-heng. Chemical Kinetics of Carbon Isotope Fractionation of Oil-Cracking Methane and Its Initial Application[J]. J4, 2006, 36(05): 825 -829 .
[4] DING Zhi-hong,FENG Ping,MAO Hui-hui. Research and Application of a Method Considering Runoff Distribution Through A Year During Partitioning Runoff into Abundant and Low State[J]. J4, 2009, 39(2): 276 -0280 .
[5] LI Song, TANG Da-zhen, WANG Wei, XU Hao, YANG Zi, CHEN Xiao-zhi, CUI Li-wei. Sequence Stratigraphic Framework and Geological Significance for Petroleum of Xishanyao Formation in Shanle Oilfield[J]. J4, 2011, 41(4): 983 -991 .
[6] ZENG Yu-chao, SU Zheng, WU Neng-you, WANG Xiao-xing, HU Jian. Temperature Distribution Characteristics of Bedrock Fracture Groundwater System at Zhangzhou Geothermal Field[J]. J4, 2012, 42(3): 814 -820 .
[7] He Jun, Ye Xueyan. Probability Design of Thickness of Composite Liners Based on Organic Pollutant Diffusion[J]. Journal of Jilin University(Earth Science Edition), 2013, 43(1): 228 -234 .
[8] LI Jian-ping, LI Tong-lin, ZHANG Hui, XU Kai-jun. Study and Application of the TEM Forward and Inversion Problem of Irregular Loop Source over the Layered Medium[J]. J4, 2005, 35(06): 790 -0795 .
[9] ZHONG Yu-hong,FANG Chun-sheng,QIU Li-min, LV Li-sha, ZHANG Zi-yi, DONG De-ming,YU Lian-gui, LIU Hui, LIU Chun-yang, SU Hong-shi, ZHAO Jing. Application of Electron Microscopic Analysis for the Sources Apportionment of Atmospheric Particles[J]. J4, 2008, 38(3): 473 -0478 .
[10] LIU Jun-lai, TANG Yuan, SONG Zhi-jie, Tran My Dung, ZHAI Yun-feng, WU Wen-bin, CHEN Wen. The Ailaoshan Belt in Western Yunnan:Tectonic Framework and Tectonic Evolution[J]. J4, 2011, 41(5): 1285 -1303 .