首页 | 本学科首页   官方微博 | 高级检索  
     

凤凰山花岗岩体构造系统分析及侵位机制
引用本文:李东旭,张达,刘文灿,杜子图. 凤凰山花岗岩体构造系统分析及侵位机制[J]. 地质力学学报, 1996, 2(2): 55-65
作者姓名:李东旭  张达  刘文灿  杜子图
作者单位:1. 中国地质大学, 北京;
基金项目:本文得到矿部地质力学开放研究实验室资助
摘    要:本文从宏观上对凤凰山岩体的区域构造位置、岩体侵位前后的构造演化过程及岩浆侵位时的动力学条件进行了论述;对岩体内部及接触带的面理、线理进行了磁组构测量、显微构造观察、包体应变测量及X光组构分析等系统研究,最终获得如下结论:该岩体侵位除有膨胀作用外,在岩体侵位后期还有过旋转运动,而且岩体侵位受到NNE向左旋剪切作用控制。 

关 键 词:凤凰山   岩体内部构造   接触带构造   侵位机制

TECTONIC SYSTEM ANALYSIS OF THE FENGHUANG SHAN INTRUSIVE AND ITS EMPLACEMENT
Li Dongxu,Zhang D,Liu Wengcan and Du Zitu. TECTONIC SYSTEM ANALYSIS OF THE FENGHUANG SHAN INTRUSIVE AND ITS EMPLACEMENT[J]. Journal of Geomechanics, 1996, 2(2): 55-65
Authors:Li Dongxu  Zhang D  Liu Wengcan  Du Zitu
Affiliation:1. China University of Geosciences Beijing;2. Institute of Geomechanics, CAGS
Abstract:In this paper, a discussing is made of the location of the Fenghuanshan pluton, in the regional tectonic regime, tectonic evolution before and after the emplacement and the dynamic conditions for the magma emplacement. The foliations and lineations both in the pluton and in the contact zone are systematically studied by measuring their magnetic fabrics, microstructures, strained inclusions and X-ray analysis of rock fabrics. As a result, it leads to the conclusion that there occurred not only dilatation due to the emplacement but also rotation of the intrusive in the late stage of the emplacement, which was controlled by the NNE sinistralshear.
Keywords:Emplacement of the Fenghuangshan pluton  magnetic fabrics
本文献已被 维普 等数据库收录!
点击此处可从《地质力学学报》浏览原始摘要信息
点击此处可从《地质力学学报》下载全文
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号