盆地研究中不整合成因分析

被引:27
作者
程日辉
林畅极
刘景彦
机构
[1] 中国地质大学能源系!北京
关键词
沉积盆地; 不整合; 成因分析;
D O I
暂无
中图分类号
P542 [构造运动];
学科分类号
070904 ;
摘要
沉积盆地的不整合使地层记录是非连续性。不整合的时空型式可以反映出不整合的成国。不整合成因分析不仅是对不整合形成的主要方式——侵蚀(包括陆上暴露侵蚀和水下侵蚀)和非侵蚀作用的研究,而且对其控制因素如大陆抬升、海平面变化以及盆地构造活动等进行分析。本文在对不整合研究进行历史回顾的基础上介绍了近来有关对不整合成因分析的认识和一些分析方法。
引用
收藏
页码:23 / 27
页数:5
相关论文
共 7 条
[1]  
Wemer P R.Developments in sequence stratigrphy;foreland and cratonic basin. American Association of Petroleum Geologists Bulletin . 1992
[2]  
Shaw J H,Hook S C,Sitohang E P.Extensional fault— bend folding and synrift deposion anexample from the central Sumatra basin Indonesia. American Association of Petroleum Geologists Bulletin . 1997
[3]  
Visher S.Exploration stratigraphy. . 1984
[4]  
Schager W.Deposional basin and environmental change-important factors in sequence stratigaphy. Sedimentary Geology . 1991
[5]  
wail P R,Hardenbol J,Todd R G.Jurassic unconformities chronostratigraphy,and sea level changesfrom seiemic stratigraphy and biostratigrphy.In:Schlee J S,ed.Interreginal unconformites andhydrocarbon accumulation. AAPG Memoir . 1984
[6]  
Sloss L L.Comparative anatomy of cratonic unconformites.In:schlee J S,ed.Interreginalunconformites and hydrocarbon accumulation. AAPG Memoir . 1984
[7]  
Einsele G,et al.Cycles and events in stratigraphy.Springer-Verlag, 19916 Vail P R. Seismic stratigraphy interpretation using sequence stratigraphy. Part 1: Seismic stratigraphyinterpretation procedure. In: Bally A W, ed. Atlas of seismic stratigraphy. American Association of Petroleum Geologists Bulletin . 1987