摘要
主要概述了伸展背景下砂质沉积物在不同构造样式下的沉积型式的研究进展。近来的研究日益表明特定的沉积型式与所处单元构造样式之间存在特定的联系。沉积盆地边缘—斜坡地区具有不同的构造样式 ,控制了砂质沉积物的沉积型式包括来源区、水流方式、砂体几何形态与分布以及沉积构成等。
The studies on the sedimentation and tectonics have revealed the special relationship between the styles of sedimentation and unit structural patterns recently.The different structural patterns developed in the margin slope areas of the sedimentary basins have the controled source area,drainage catchment,geometry and distribution of sand deposits as well as sedimentary architecture.This paper presents advances in study of the sedimentation styles of the sand deposits and their tectonic controls the structural patterns.
出处
《地质科技情报》
CAS
CSCD
北大核心
2000年第1期11-15,共5页
Geological Science and Technology Information
基金
国家自然科学基金项目!( 4 95 72 12 0 )
