吉林大学学报(地球科学版) ›› 2015, Vol. 45 ›› Issue (2): 374-388.doi: 10.13278/j.cnki.jjuese.201502104

• 地质与资源 • 上一篇    下一篇

嫩江黑河构造带收缩与伸展——源自晚古生代花岗岩类的地球化学证据

汪岩1, 付俊彧1, 杨帆1, 那福超1, 陈会军1, 张昱2, 杨晓平3, 张铁安2   

  1. 1. 沈阳地质矿产研究所/中国地质调查局沈阳地质调查中心, 沈阳 110034;
    2. 黑龙江省区域地质调查所, 哈尔滨 150080;
    3. 黑龙江省地质调查研究总院齐齐哈尔分院, 哈尔滨 150036
  • 收稿日期:2014-06-15 发布日期:2015-03-26
  • 作者简介:汪岩(1968-),男,教授级高级工程师,主要从事区域地质与矿产调查研究工作,E-mail:wy68413@163.com
  • 基金资助:

    中国地质调查局地质大调查项目(12120114019601,1212011220435,12120114085601)

Contraction and Extension in Nenjiang-Heihe Tectonic Belt: Evidence from the Late Paleozoic Granitoid Geochemistry

Wang Yan1, Fu Junyu1, Yang Fan1, Na Fuchao1, Chen Huijun1, Zhang Yu2, Yang Xiaoping3, Zhang Tiean2   

  1. 1. Shenyang Institute of Geology and Mineral Resources/Shenyang Center of Geological Survey, China Geological Survey, Shenyang 110034, China;
    2. Heilongjiang Province Institute of Regional Geology Survey, Harbin 150080, China;
    3. Qiqihar Branch, Heilongjiang Research Insitute of Geological Survey, Harbin 150036, China
  • Received:2014-06-15 Published:2015-03-26

摘要:

黑龙江省嫩江至黑河一带发育大量的晚古生代花岗岩类岩石,同位素测年结果显示主要集中在3个时代:早石炭世、晚石炭世和早二叠世。岩石类型从花岗闪长岩-二长花岗岩-正长花岗岩-碱长花岗岩等均有不同出露,石炭纪部分岩石遭受韧性剪切变质变形作用改造形成花岗质糜棱岩。岩石整体具有高硅、富钾钠特征;稀土元素总量偏高,铕负异常明显;微量元素具明显的大离子亲石元素(LILE)K、Rb、Th富集和高场强元素(HFSE)Nb、P、Ti亏损特征。其中石炭纪花岗岩类地球化学特征显示陆缘弧及同碰撞花岗岩特点,二叠纪花岗岩则表现后造山花岗岩特点。二者反映了由碰撞造山向板内后造山阶段转变的构造环境特点,也反映了嫩江-黑河构造带汇聚拼合与伸展的活动史。

关键词: 花岗岩类, 地球化学, 晚古生代, 嫩江-黑河构造带

Abstract:

We present the geochemical characteristics of the Late Paleozoic granitoid in Heilongjiang Nenjiang-Heihe through the study on the different types of granitoid. The isotopic dating results provide three time periods for these granitoids: Early Carboniferous,Late Carboniferous, and Early Permian.The granitoids are rich in silica, potassium, and sodium;and also the rare-earth elements relatively with significant negative Eu anomaly. The trace elements are typically rich in large ion lithophile element (LILE)K, Rb, Th, but poor with high-field-strength element (HFSE) Nb, P, Ti. The existence of granitic mylonite reflects its deformation and metamorphism through tuctile shear. Based on the above, the Carboniferous granitoid experienced a continental margi arc syn-collision; while the Permian granites deformed under a post-orogenesis These two reflects anenvironmental transition from a tectonic collision to an intraplate post-orgenesis, and also the activity history of genesis, convergece, andextension of the Nenjiang-Heihe tectonic belt.

Key words: granitoid, geochemistry, Late Paleozoic, Nenjiang-Heihe tectonic belt

中图分类号: 

  • P588.12

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