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川西龙门山中段彭州式铜矿区构造体系及与成矿的关系
引用本文:杨钻云,刘肇昌,钟康慧,邱仁轩,秦术凯,王乐峰.川西龙门山中段彭州式铜矿区构造体系及与成矿的关系[J].大地构造与成矿学,2010,34(2).
作者姓名:杨钻云  刘肇昌  钟康慧  邱仁轩  秦术凯  王乐峰
作者单位:成都理工大学,沉积研究院,四川,成都,610059;四川省冶金地质勘查局六○六大队,四川,彭州,611930;成都理工大学,沉积研究院,四川,成都,610059;四川省冶金地质勘查局六○六大队,四川,彭州,611930
基金项目:全国矿产资源潜力评价项目 
摘    要:川西龙门山中段彭州式铜矿形成于岛弧构造环境,其形成经历了晋宁期幔源火山沉积和褶皱变形、印支期-燕山期以来强烈的构造挤压和破坏。根据研究区地层形变的各种构造形迹,将区内构造体系划分为北北西向"多"字型和北东向华夏式两种构造体系。"多"字型构造体系是在晋宁期右行剪切作用下形成北东—北北东向的褶皱带,后经印支期-燕山期以来的左行旋转至北北西而保留至今,表现为黄水河群组成的复式背、向斜褶皱带;华夏式构造体系显示了印支期以来北东—南西方向强大的挤压,表现为前期的叠瓦状断裂和后期的"飞来峰"构造。两种构造体系共同控制着彭州式铜矿床的形成及改造。根据二者的平面展布形态、构造出露特征及其动力学标志,将其划分为包容和交接两种复合关系,即"多"字型构造体系包容于华夏式构造体系中,在研究区南部二者呈反接关系。

关 键 词:构造体系  旋转  包容  反接

Relationship Between Tectonic System and Mineralization on the Pengzhou-type Copper Ore District in the Middle of Longmen Mountains, Western Sichuan
YANG Zuanyun,LIU Zhaochang,ZHONG Kanghui,QIU Renxuan,QIN Shukai,WANG Lefeng.Relationship Between Tectonic System and Mineralization on the Pengzhou-type Copper Ore District in the Middle of Longmen Mountains, Western Sichuan[J].Geotectonica et Metallogenia,2010,34(2).
Authors:YANG Zuanyun  LIU Zhaochang  ZHONG Kanghui  QIU Renxuan  QIN Shukai  WANG Lefeng
Institution:YANG Zuanyun1,2,LIU Zhaochang1,ZHONG Kanghui1,QIU Renxuan2,QIN Shukai2 and WANG Lefeng2(1.Institute of Sedimentation,Chengdu University of Technology,Chengdu 610059,Sichuan,China,2.No.606 Team of Sichuan Bureau of Metallurgy and Geology Exploration,Pengzhou 611930,China)
Abstract:The Pengzhou copper mine area in the middle section of Longmenshan mountains was formed in an island-arc tectonic environment. During its formation,it undergone the mantle-derived volcanic desposition and deformation of folds in the Jinning period,and Indosinian-Yanshannian strong tectonic compression and destruction. According to the different tectonic systems,the studied area can be devided into two kinds of tectonic systems:the NNW-trending multifont style and NE-trending cathaysoid style. The multifont ...
Keywords:tectonic system  rotation  inclusive  reverse  Longmen mountains  Pengzhou-type copper  
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