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黔桂地区泥盆纪层序地层和台内裂陷槽的形成演化
引用本文:杜远生,冯庆来.黔桂地区泥盆纪层序地层和台内裂陷槽的形成演化[J].沉积学报,1997,15(4):11-17.
作者姓名:杜远生  冯庆来
作者单位:1 中国地质大学,武汉 430074;
基金项目:国家基础性研究重大关键项目SSLC和高等学校博士学科点专项科研基金(9549111)联合资助
摘    要:黔桂地区是泥盆纪时期南华海盆内裂陷活动作用初始且十分显著的地区。本文结合区域构造和盆地格局分析,通过典型剖面研究,将黔桂稳定型滨岸一台地相区的泥盆系划分为21个3级海平面变化控制的层序。根据南丹罗富、大厂裂陷槽盆地泥盆系层序地层研究和与相邻稳定型泥盆系层序地层对比及层序地层格架分析,揭示了裂陷槽盆地的形成演化过程。指出构造幕式沉降是裂陷槽盆地层序发育和层序构成的主控因素。

关 键 词:华南    泥盆系    层序地层    裂陷槽
收稿时间:1996-08-27

Devonian Sequence Stratigrapny and Formation and Evolution of Intraplatform Rift Trough in the Guangxi and Guizhou Area,China
Institution:1 China University of Geosciences,Wuhan,430074;2 Geological Institute of Guang Xi,Nanning,530023
Abstract:Guangxi and Guizhou in South Ghina are one of the famous Devonian distribution areas interestedby both Chinese and foreign geologists.By classification and correlation of sequence stratigraphy of morethan 10 sections in Guizhou and Guangxi.21 sequences and T- Rcycles were identified to correspond tothird- order sea- level changes.On the basis of the division, correlation and study of the framework ofsequences in the stable regions and rift trough in the Luofu, Dachang sections, Nandan County, the for-mation and evolution of the rift trough.Episodic tectono- setting mainly controlled the development andarchitectures of sequences in the rift trough were discussed.Episodic tectono- sequences recorded thedepositional response to the episodic tectono- setting of the rift trongh.
Keywords:, South China,Devonian,sequence,rift trough,
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