非洲中南部赞比西造山带地质演化及矿产资源现状

P548; 赞比西造山带位于非洲中南缘,是新元古代-早古生代泛非造山运动的重要组成部分,形成于冈瓦纳古陆中心陆块缝合期间.赞比西带大地构造位置位于刚果克拉通和卡拉哈里克拉通之间,东连莫桑比克带,北接卢弗里安弧,西部和纳米比亚的达马拉构造带相呼应.带内主要地层单元为基底杂岩和一套沉积在硅铝质基底上的浅变质沉积序列.岩石学及构造学证据证明沉积作用发生在陆内裂谷盆地中,大量同位素年龄限制了盆地演化时代大致为880～820Ma;赞比西带在600～450Ma的泛非造山事件中再次活化,韧性剪切和大范围糜棱岩化导致了角闪岩相变质作用和同构造期花岗质岩体侵入事件同时发生.赞比西带目前已发现的矿产包括岩浆通道型...

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Published in地质与勘探 Vol. 55; no. 6; pp. 1549 - 1558
Main Authors 邢仕, 纪山青, 杜明龙, 任军平, 刘子江, 古阿雷, 孙宏伟
Format Journal Article
LanguageChinese
Published 河北省地矿局第五地质大队,河北唐山,063000%中国地质调查局天津地质调查中心,天津,300170 01.11.2019
Subjects
赞比西造山带
地质演化
硅锌矿
非洲中南部
镍硫化物矿床
Online AccessGet full text
ISSN0495-5331
DOI10.12134/j.dzykt.2019.06.021

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Abstract P548; 赞比西造山带位于非洲中南缘,是新元古代-早古生代泛非造山运动的重要组成部分,形成于冈瓦纳古陆中心陆块缝合期间.赞比西带大地构造位置位于刚果克拉通和卡拉哈里克拉通之间,东连莫桑比克带,北接卢弗里安弧,西部和纳米比亚的达马拉构造带相呼应.带内主要地层单元为基底杂岩和一套沉积在硅铝质基底上的浅变质沉积序列.岩石学及构造学证据证明沉积作用发生在陆内裂谷盆地中,大量同位素年龄限制了盆地演化时代大致为880～820Ma;赞比西带在600～450Ma的泛非造山事件中再次活化,韧性剪切和大范围糜棱岩化导致了角闪岩相变质作用和同构造期花岗质岩体侵入事件同时发生.赞比西带目前已发现的矿产包括岩浆通道型镍硫化物矿床和浅成低温热液型硅锌矿等.笔者通过对赞比西带的地质演化和矿床成矿作用进行系统总结,并将赞比西带内的主要矿床和国内类似矿床进行对比分析,以期为赞比西带找矿实践提供依据或线索.
AbstractList P548; 赞比西造山带位于非洲中南缘,是新元古代-早古生代泛非造山运动的重要组成部分,形成于冈瓦纳古陆中心陆块缝合期间.赞比西带大地构造位置位于刚果克拉通和卡拉哈里克拉通之间,东连莫桑比克带,北接卢弗里安弧,西部和纳米比亚的达马拉构造带相呼应.带内主要地层单元为基底杂岩和一套沉积在硅铝质基底上的浅变质沉积序列.岩石学及构造学证据证明沉积作用发生在陆内裂谷盆地中,大量同位素年龄限制了盆地演化时代大致为880～820Ma;赞比西带在600～450Ma的泛非造山事件中再次活化,韧性剪切和大范围糜棱岩化导致了角闪岩相变质作用和同构造期花岗质岩体侵入事件同时发生.赞比西带目前已发现的矿产包括岩浆通道型镍硫化物矿床和浅成低温热液型硅锌矿等.笔者通过对赞比西带的地质演化和矿床成矿作用进行系统总结,并将赞比西带内的主要矿床和国内类似矿床进行对比分析,以期为赞比西带找矿实践提供依据或线索.
Author 任军平
古阿雷
邢仕
杜明龙
刘子江
孙宏伟
纪山青
AuthorAffiliation 河北省地矿局第五地质大队,河北唐山,063000%中国地质调查局天津地质调查中心,天津,300170
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Author_FL REN Junping
SUN Hongwei
JI Shanqing
GU Alei
DU Minglong
LIU Zijiang
XING Shi
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Keywords 赞比西造山带
地质演化
硅锌矿
非洲中南部
镍硫化物矿床
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Title 非洲中南部赞比西造山带地质演化及矿产资源现状
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