Journal of Jilin University(Earth Science Edition) ›› 2021, Vol. 51 ›› Issue (4): 1098-1118.doi: 10.13278/j.cnki.jjuese.20210031

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Geochronology,Geochemistry and Tectonic Significance of the Monzonitic Granites of Maoershan Pluton from the Southern Zhangguangcai Range in Heilongjiang Province, China

Zhao Yue1,2, Liu Jingdang2, Zhang Guobin2, Zhang Yanfei2,3   

  1. 1. Institute of Innovation and Development for Fuxin Transition, Liaoning Technical University, Fuxin 123000, Liaoning, China;
    2. Mining Institute, Liaoning Technical University, Fuxin 123000, Liaoning, China;
    3. Shenyang Center of Geological Survey, China Geological Survey, Shenyang 110034, China
  • Received:2021-01-26 Online:2021-07-26 Published:2021-08-02
  • Supported by:
    Supported by the Fund of the Department of Science and Technology of Liaoning Province (20170540428), the Fund of Educational Department of Liaoning Province (LJ2019JL027) and "Nurturing Seedlings" Project of Young Science and Technology Talents of the Department of Education of Liaoning Province (LJ2020QNL003)

Abstract: The Zhangguangcai Range is a collision orogenic belt between the Songnen massif and the Jiamusi massif, and is an important part of the "Giant Granite Province" in Northeast China. Based on zircon U-Pb dating and petrogeochemical analysis, we have studied the chronology, geochemical characteristics and tectonic setting of the Early Jurassic monzogranites in the southern Zhangguangcai Range. The zircon U-Pb dating results show that the diagenetic age of the fine-grained monzogranite granite sample is (176.4±1.1) Ma; The medium-grained monzogranite samples are(178.9±1.3)Ma,(177.7±1.1)Ma; The coarse-grained monzogranite samples are(180.0±1.8)Ma, (179.9±1.2)Ma. These ages belong to the Early Jurassic. Petrogeochemical results show that the fine-grained monzogranite samples, medium-grained monzogranite samples and coarse-grained monzogranite samples are rich in silicon, poor in aluminum, high in alkali, low in calcium, enriched in Zr, Hf, Rb, K, depleted in Ba, Sr, Nb, P, Ti, swallow-type rare earth distribution model and other characteristics, the diagenetic type belongs to post-orogenic A2 granite. Combining the characteristics of chronology and geoch emistry, the authors believe that the Early Jurassic monzonitic granite in the study area was formed in the post-collision tectonic setting, representing an extension during the collision-assembly process of the Jiamusi and Songnen blocks, indicating the Early Jurassic the regional tectonic environment gradually changed from compression orogenic to post-orogenic extensional environment.

Key words: Zhangguangcai Range, Early Jurassic, monzogranite, zircon U-Pb dating geochemistry, petrogenesis, tectonic setting

CLC Number: 

  • P588.1
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[4] ZHAO Hong-guang,SUN Jing-gui, CHEN Jun-qiang,ZHAO Jun-kang, YAO Feng-liang,DUAN Zhan. The Genesis and Evolution of Orebearing Fluids of the Xiaoxinancha Goldbearing Porphyry Copper Deposit in Yanbian Area: H,O,C,S,Pb Isotope Tracing[J]. J4, 2005, 35(05): 601 -606 .
[5] MENG Yuan-lin,GAO Jian-jun,LIU De-lai, NIU Jia-yu,SUN Hong-bin,ZHOU Yue,XIAO Li-hua,WANG Yue-chuan. Diagenetic Facies Analysis and Anomalously High Porosity Zone Prediction of the Yuanyanggou Area in the Liaohe Depression[J]. J4, 2006, 36(02): 227 -0233 .
[6] ZENG Zhao-fa, WU Yan-gang, HAO Li-bo,WANG Zhe-jiang,HUANG Hang. The Poisson’s Theorem Based Analysis Method and Application of Magnetic and Gravity Anomalies[J]. J4, 2006, 36(02): 279 -0283 .
[7] CHANG Qiu-ling, LU Xin-xiang, LIU Dong-hua, LI Ming-li. The Relation Between Gold Deposits and Wuduoshan Granite in Eastern Qinling[J]. J4, 2006, 36(03): 319 -325 .
[8] MA Yan-mei,CUI Qi-liang,ZHOU Qiang,HUANG Wei-jun,LIU Ye,PENG Gang,ZOU Guang-tian. InSitu Raman Study of Olivine Under High Temperature[J]. J4, 2006, 36(03): 342 -345 .
[9] YIN Wen,YIN Xing-yao,ZHANG Fan-chang. A Study on Seismic Attribute Optimization Based on Parallel Genetic Algorithm[J]. J4, 2005, 35(05): 672 -676 .
[10] WEI Xi, DENG Jin-fu,CHEN Yi-han. Distribution Characters and Exploration Potential of Mesozoic Sea Facies Sedimentary Strata in the South China Sea Basin[J]. J4, 2005, 35(04): 456 -0461 .