中新世以来滇藏怒江峡谷区变形与构造深度层次
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  • 英文篇名:Crustal deformation and tectonic levels of Nujiang Gorge since the Miocene
  • 作者:刘志成 ; 季建清 ; 洒骁 ; 陈亚鹏 ; 钟大赉
  • 英文作者:Liu Z C;Ji J Q;Sa X;Chen Y P;Zhong D L;
  • 关键词:构造层次 ; 怒江 ; 流动变形 ; 韧性变形 ; 热史演化
  • 中文刊名:JDXK
  • 英文刊名:Scientia Sinica(Terrae)
  • 机构:中国地震灾害防御中心;北京大学地球与空间科学学院;中国电建集团北京勘探设计研究院有限公司;中国科学院地质与地球物理研究所;
  • 出版日期:2018-01-20
  • 出版单位:中国科学:地球科学
  • 年:2018
  • 期:v.48
  • 基金:中国地质调查局项目(编号:12120113013700);; 中国地震灾害防御中心主任基金项目(编号:201604)资助
  • 语种:中文;
  • 页:JDXK201801005
  • 页数:17
  • CN:01
  • ISSN:11-5842/P
  • 分类号:66-82
摘要
地壳不同深度上的岩石物理性质的差异决定了在垂向上的构造变形呈现不同构造样式.依据地壳内主导变形机制的差异,划分出不同的构造层次,有助于更好地解析出露地质体的构造演化.滇藏怒江峡谷区具有高差大,河流切割地壳深度大,以及在强烈的变形下不同地壳层次的岩石得以出露等独特特征,因此是地壳变形层次研究的理想区域.本文通过对怒江流域察瓦龙至福贡区段的详细区域地质考察和构造变形分析,识别出地壳深层次到浅层次的不同构造变形样式.其中,深层次的构造样式以流动构造变形为主,主要出露于马吉地区.韧性变形在整个研究区广泛出露.高黎贡右行走滑剪切带和普拉底-松塔左行走滑剪切带分别出露在马吉南北区域.以相似褶皱和近直立密集劈理为特征的构造变形样式发育在普拉底以北.脆性断裂,为浅层次变形样式,叠加改造了较深层次变形,在整个研究区都有广泛发育.因此,研究区的主要构造样式由深至浅可划分为流变构造、韧性剪切构造、相似褶皱和脆性断裂构造4个构造层次.4个构造层次不同变形样式的发育均与北东东-南西西向挤压应力场有关.结合热史演化和区域构造特征,滇藏怒江峡谷区不同深度层次构造样式的发育与中新世(21Ma)以来地壳差异性隆起或者剥露有密切的关系.
        
引文
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