1.
Sedimentary Response to Permian Structural Movements in Wuxia Foreland Thrust Belt of Junggar Basin
准噶尔盆地乌夏前陆冲断带构造活动—沉积响应
2.
Salt tectonic evolution and hydrocarbon accumulation of Kuqa foreland fold belt, Tarim Basin, NW China.
库车前陆褶皱-冲断带前缘大型盐推覆构造。
3.
Seismic Imaging Tenhique Study on Complex Tectonic Structure in Thrust Fault Foreland Basin;
前陆冲断带复杂构造地震成像技术研究
4.
Meso-Cenozoic Evolution of Dabashan Foreland Basin-thrust Belt, Central China;
中—新生代大巴山前陆盆地—冲断带的形成演化
5.
Balanced Cross-sections of Salt Structures in Kuqa Foreland Thrust Belt in Northern Part of Tarim Basin
库车前陆冲断带盐构造区平衡剖面研究
6.
Wuxia fault belt in the eastern part of northwestern margin of Junggar basin is an important part in the thrust belt of the northwestern margin.
乌夏断裂带位于准噶尔盆地西北缘的东部，是西北缘冲断带的一个重要组成部分。
7.
EVOLUTION OF STRUCTURAL STYLE IN WUXIA FAULT BELT IN JUNGGAR BASIN
准噶尔盆地乌夏断裂带构造样式演化
8.
Research on the Foreland Thrust Belt and on the Accumulation of Petroleum in the North-Western Margin of the Jungger Basin, China;
准噶尔盆地西北缘前陆冲断带特征及对油气聚集作用的研究
9.
Geometrical Types,Distribution Characteristics and Genetic Mechanism of Structural Deformation in Southern Dabashan Foreland Fold-Thrust Belt,Central China
南大巴前陆冲断带构造变形几何类型、分布特征及其成因分析
10.
The Tectonic Segmentation and Hydrocarbon Exploration of the Foreland Thrust Belt in the Northwestern Tarim Basin
塔里木盆地西北缘前陆冲断带构造分段特征及勘探方向
11.
Seal capacity of caprock and its control effect on hydrocarbon in the foreland thrust belt of Jungar basin
准噶尔南缘前陆冲断带盖层封闭能力及其对油气的控制作用
12.
Research on Seismic Methods of Reservoir Prediction & Evaluation in Wu-Xia Fault Zone;
乌—夏断裂带储层预测与评价地震方法研究
13.
The distribution regularity and master control agency of the Permian oil play in the Wuxia fracture belt in Wuxia fracture belt,Zhunge'er Basin
准噶尔盆地西北缘乌夏断裂带二叠系油气成藏组合
14.
Geochemical Features of Fluid Activity in Wuxia Fault Belt of Junggar Basin
准噶尔盆地乌-夏断裂带流体活动的地球化学特征
15.
Study on the structural features and hydrocarbon accumulation modes of Wuxia fault belt in the northwest margin of Junggar Basin
准噶尔盆地西北缘乌夏断裂带构造特征与油气成藏模式
16.
Research on the Tectogenetic Movement and the Fluid Migration in Dabashan Thrust and Fold Belt and Its Foreland;
大巴山冲褶带及前陆构造活动与流体运移研究
17.
Continent to continent collisions along subduction zones makes continents larger, while rifts along spreading centers break them apart again.
大陆与大陆沿俯冲带的碰撞使大陆扩大，而沿扩张中心的断陷使它们再次分开。
18.
LOWER PALEOZOIC OMISSION ZONE IN JIANGNAN UPLIFT──A SIGN OF CALEDONIAN FORELAND FOLD THRUST BELT
江南隆起上的下古生界缺失带──华南加里东前陆褶冲带的标志