兰坪盆地侏罗纪陆相层序地层研究  

ON JURASSIC CONTINENTAL SEQUENCE STRATIGRAPHY OF THE LANPING BASIN

作　　者：朱利东[1] 刘登忠[1] 王国芝[1] 陶晓风[1] 徐新煌[1] 李佑国[1] 

机构地区：[1]成都理工学院,四川成都610059

出　　处：《地层学杂志》2001年第1期40-43,共4页Journal of Stratigraphy

基　　金：国土资源部资源与环境科技攻关项目《兰坪盆地演化与成矿关系研究》课题及兰坪等3幅1/5万区调项目研究成果

摘　　要：陆相盆地与海相盆地 (尤其是陆棚海盆地 )的沉积充填具有着不同的主控因素 ,构造的控制作用在陆相盆地中尤为重要。陆相盆地的层序地层划分依据为构造作用的转化面划分为构造层序 ,构造层序内部依据沉积充填样式的差异进一步划分出层序。兰坪盆地的侏罗系共划分出一个构造层序和The sedimentary fillings of continental and marine basins (especially shelf basin) were caused by different control factors. The tectonic control is very important in continental basin. According to the features of the continental basin, the sequence stratigraphic division of the continental basin is put forward. That is why the tectonic sequence is divided by the change face of construction effect and the sequence in construction is divided on the basis of the sedimentary filling pattern. This paper divides the Jurassic of the Lanping Basin into one construction sequence and three sequences.

关 键 词：兰坪盆地 侏罗系 陆相层序地层 构造层序 层序 

分 类 号：P534.52[天文地球—古生物学与地层学] P539.2[天文地球—地质学]