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桂西右江盆地伸展构造特征

张能, 黄启明, 谭建政, 李江

张能, 黄启明, 谭建政, 李江. 桂西右江盆地伸展构造特征[J]. 中国地质, 2016, 43(3): 953-968. DOI: 10.12029/gc20160318
引用本文: 张能, 黄启明, 谭建政, 李江. 桂西右江盆地伸展构造特征[J]. 中国地质, 2016, 43(3): 953-968. DOI: 10.12029/gc20160318
ZHANG Neng, HUANG Qi-ming, TAN Jian-zheng, LI Jiang. Extensive structural characteristics of Youjiang Basin, western Guangxi[J]. GEOLOGY IN CHINA, 2016, 43(3): 953-968. DOI: 10.12029/gc20160318
Citation: ZHANG Neng, HUANG Qi-ming, TAN Jian-zheng, LI Jiang. Extensive structural characteristics of Youjiang Basin, western Guangxi[J]. GEOLOGY IN CHINA, 2016, 43(3): 953-968. DOI: 10.12029/gc20160318

桂西右江盆地伸展构造特征

基金项目: 

中国地质调查局项目"广西区域地质调查片区总结与服务产品开发"(12120113012600)及2015年第二批广西找矿突破战略行动地质矿产勘查项目"广西右江盆地演化与成矿关系研究"联合资助。

详细信息
    作者简介:

    张能,男,1967年生,博士,高级工程师,从事区域地质调查与找矿研究;E-mail:1173938529@qq.com。

  • 中图分类号: P542

Extensive structural characteristics of Youjiang Basin, western Guangxi

Funds: 

Supported by Guangxi Regional Geological Survey Area Summary and Service Product Development Project (No. 12120113012600) and The Second Batch of Prospecting Breakthrough Strategic Action Geological Mineral Exploration Project in 2015, Guangxi "Youjiang Guangxi Basin Evolution and Metallogenic Relationship Research".

  • 摘要: 桂西右江盆地属扬子陆块西南缘晚古生代—中生代复合型裂谷盆地,在区域引张体制下,呈现盆-台相间、堑-垒式断块构造等以伸展作用为主的构造格局。台缘斜坡环境二叠纪海绵礁、同沉积角砾岩带和浊积岩系等构造-沉积事件层发育;台内及边缘以上泥盆统与下石炭统、上石炭—下二叠统与中二叠统、中二叠统与上二叠统、下三叠统与中三叠统之间为主的平行或微角度或超覆不整合,分别反映了柳江、黔桂、东吴、桂西伸展不整合构造运动事件。文章旨在通过该盆地晚古生代—三叠纪伸展构造特征的总结,为深入探讨其动力学背景及演化机制提供有益的参考。
    Abstract: The Youjiang Basin in western Guangxi is a late Paleozoic-Mesozoic compound rift basin on the southwestern margin of Yangtze landmass. Under the regional extensional system, there appears the structural framework of extension-dominated alternate basin- platform and horst- graben style fault block structure. Structural- sedimentary event layers such as Permian sponge reefs, synsedimentary breccias belt and turbidite series are well developed, suggesting a marginal platform slope environment. In the interior or on the margin of the platform, there are parallel, micro- angle or overlap unconformities dominantly between upper Devonian and lower Carboniferous, between upper Carboniferous—lower Permian and middle Permian, between upper Permian and middle Permian, and between lower Triassic and middle Triassic strata, which respectively reflect four unconformable structural events of Liujiang orogeny, Qiangui epiorogenic event, Dongwu revolution, and Guixi movement. Based on the summarization of Late Paleozoic-Triassic extensive structural features of the Youjiang Basin, this study aims at providing useful reference for the investigation of the dynamics background and evolution mechanism of the Youjiang Basin, western Guangxi.
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出版历程
  • 收稿日期:  2015-08-28
  • 修回日期:  2015-09-25
  • 网络出版日期:  2023-09-26
  • 刊出日期:  2016-06-24

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