吉林大学学报(地球科学版) ›› 2021, Vol. 51 ›› Issue (4): 1098-1118.doi: 10.13278/j.cnki.jjuese.20210031

• 地质与资源 • 上一篇    下一篇

张广才岭南部帽儿山岩体二长花岗岩年代学、地球化学特征及其构造意义

赵越1,2, 刘敬党2, 张国宾2, 张艳飞2,3   

  1. 1. 辽宁工程技术大学阜新转型创新发展研究院, 辽宁 阜新 123000;
    2. 辽宁工程技术大学矿业学院, 辽宁 阜新 123000;
    3. 中国地质调查局沈阳地质调查中心, 沈阳 110034
  • 收稿日期:2021-01-26 出版日期:2021-07-26 发布日期:2021-08-02
  • 作者简介:赵越(1995-),男,讲师,博士,主要从事矿产勘查方面的研究,E-mail:zhaoyue9501@163.com
  • 基金资助:
    辽宁省科技厅基金项目(20170540428);辽宁省教育厅面上基金项目(LJ2019JL027);辽宁省教育厅青年科技人才"育苗"项目(LJ2020QNL003)

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)

摘要: 张广才岭是松嫩地块与佳木斯地块之间的碰撞造山带,是东北"巨型花岗岩省"的重要组成部分。本文通过锆石U-Pb定年和岩石地球化学分析,研究了张广才岭南部帽儿山二长花岗岩年代学、地球化学特征和构造背景。锆石U-Pb年代学结果显示:张广才岭南部细粒二长花岗岩成岩年龄为(176.4±1.1)Ma,中粒二长花岗岩成岩年龄为(178.9±1.3)、(177.7±1.1)Ma,粗粒二长花岗岩成岩年龄为(180.0±1.8)、(179.9±1.2)Ma,成岩时代均属于早侏罗世。岩石地球化学研究显示:细粒二长花岗岩、中粒二长花岗岩和粗粒二长花岗岩均具有富硅、贫铝、高碱、低钙,富集Zr、Hf、Rb、K,亏损Ba、Sr、Nb、P、Ti,燕式型稀土配分模式等特征,成岩类型属于造山后A2型花岗岩。结合年代学和地球化学特征,研究区早侏罗世二长花岗岩形成于碰撞后构造背景,代表佳木斯地块和松嫩地块碰撞—拼合过程中的一次伸展作用,表明早侏罗世区域构造环境逐渐由挤压造山向造山后伸展环境转变。

关键词: 张广才岭, 早侏罗世, 二长花岗岩, 锆石U-Pb定年, 地球化学, 岩石成因, 构造背景

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

中图分类号: 

  • P588.1
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