首页 | 本学科首页   官方微博 | 高级检索  
     

鄂东南小岩体分布及其基本特征
引用本文:刘晓妮,孔繁河,杨培,刘忠明,朱琳,李红. 鄂东南小岩体分布及其基本特征[J]. 资源环境与工程, 2009, 23(4): 390-395
作者姓名:刘晓妮  孔繁河  杨培  刘忠明  朱琳  李红
作者单位:湖北省地质科学研究所,湖北,武汉,430022;湖北省第二地质大队,湖北,恩施,445000
摘    要:鄂东南燕山期小岩体(群)有137处,主要分布在两大层间顺层滑脱拆离带中和毛铺-两剑桥断裂及其附近.小岩体规模小,埋藏浅,形态多为筒状、似直立柱体、蘑菇状、脉状、岩株状、岩墙状.小岩体产状总体倾向南、南东,倾角30°以上.鄂东南小岩体主要为中酸性花岗岩类,侵入期次分为两期七次.岩浆演化从早到晚的趋势为:闪长岩、石英闪长岩、石英二长闪长玢岩、花岗闪长斑岩、花岗斑岩、石英斑岩.部分小岩体与鄂东南六大岩体一样是杂岩体,是岩浆多期次演化的产物.小岩体岩浆来源于深部,与太平洋板块向欧亚板块俯冲作用有关.

关 键 词:小岩体  基本特征  鄂东南

Distribution and Basic Characteristics of Small Intrusions in Southeast Hubei
LIU Xiaoni,KONG Fanhe,YANG Pei,LIU Zhongming,ZHU Lin,LI Hong. Distribution and Basic Characteristics of Small Intrusions in Southeast Hubei[J]. Resources Environment & Engineering, 2009, 23(4): 390-395
Authors:LIU Xiaoni  KONG Fanhe  YANG Pei  LIU Zhongming  ZHU Lin  LI Hong
Affiliation:1.Hubei Institute of Geosciences;Wuhan;Hubei 430022;2.The 2nd Geological Party;Enshi;Hubei 445000
Abstract:Small intrusions are distributed mainly in detachment structure zone between two layers,Maopu-Liangjianqiao fault and its neighbourhood in phase of Yanshan in Southeast Hubei.Small intrusions are small size,shallow buried in the form of cylinder-shape,vein,mushroom-shape,stock and dike,the attitude of small intrusions in general tend to south and southeast with a dip angle of above thirty degrees.Magma evolution trends from early to late:diorite,quartz diorite,quartz monzobiorite,granodiorite-porphyry,grani...
Keywords:small intrusions  basic characteristics  southeast Hubei  
本文献已被 CNKI 维普 万方数据 等数据库收录!
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