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1.Tarim Basin is a superimposed and composite basin of numerous proto type basins combosed of the Paleozoic cratonic basins and Meso Cenozoic foreland basins.
全面系统地总结并提出塔里木盆地10大石油地质基本特征:(1)塔里木盆地为一古生界克拉盆地与中新生界前陆盆地组成的大型叠合复合型盆地收藏指正
2.According to the characteristics of structure and sedimentation of Tarim basin, it can be divided into three assemblages i.e. pre Sinian basement structure stratigraphy, Sinian Lower Permian marine craton basin structure stratigraphy, and Upper Permian Middle Cenozoic foreland basin structure stratigraphy.
根据该盆地构造、沉积发育特征,将它划分为前震旦系基底构造-地层、震旦系—下二叠统海相克拉盆地构造-地层、上二叠统—中、新生界前陆盆地构造-地层三大组合系统。收藏指正
3.Glauconitic Condensed Sections(CS): The Key to Correlation Of Sequence Stratigraphy in the Craton Basin──Characteristics and Implication of the Cambrian Condensed Section of North China
海绿石质凝缩层-克拉盆地层序地层划分对比的关键──华北寒武系凝缩层的特征和含义收藏指正
4.CAMBRIAN DEPOSITIONAL HISTORY OF THE SIBERIAN CRATON:EVOLUTION OF THE CARBONATE PLATFORMS AND BASINS
西伯利亚克拉寒武纪沉积史:碳酸盐台地和盆地的演化收藏指正
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