1.
TECTONIC EVOLUTION OF HETIAN PALEO-UPLIFT IN TARIM BASIN AND ITS RELATION TO OIL AND GAS;
![点击朗读](/dictall/images/read.gif)
塔里木盆地和田古隆起构造演化及油气关系
2.
Research on basin-mountain tectonic-thermal history of Kongquehe Slope and Kuruketag Uplift
孔雀河斜坡与库鲁克隆起构造-热演化史研究
3.
Analasis of Relationship between Tectonic Evolution and Oil-gas in Bachu Uplift in Tarim Basin;
塔里木盆地巴楚隆起构造演化与含油气关系研究
4.
The Analyze of Tectonic Character and Favored Condition of Oil-gas Gathering in Shaya Uplift of Tarim Basin;
塔里木盆地沙雅隆起构造特征及含油气条件研究
5.
Structural Characteristics of the Xidamingshan Uplift in Guangxi and Its Relationship with the Adjacent Basins;
广西西大明山隆起构造特征及其与周缘盆地的关系
6.
Paleozoic structural styles and evolution of the North Tarim Uplift
![点击朗读](/dictall/images/read.gif)
塔北隆起古生代构造样式和构造反演
7.
The Characteristics and Physical Modeling of Extensional Structure in West Shandong Rise, China;
鲁西隆起伸展构造特征及构造物理模拟
8.
The Structural Style and Structural Evolution of Eopaleozoic in Tazhong Uplift Zone;
![点击朗读](/dictall/images/read.gif)
塔中隆起带早古生代构造样式和构造演化研究
9.
Relationship between Fractures and Preserving Disciplinarian of Gold Deposit in the Eastern Bengbu Uplift;
蚌埠隆起东端断裂构造与金矿的关系
10.
TECTONIC MECHANISM AND POOLING MODEL OF THE CALEDONIAN PALEOSWELL IN THE SICHUAN BASIN
![点击朗读](/dictall/images/read.gif)
四川盆地加里东古隆起的构造机制和成藏模式
11.
Sedimentary-structural characteristics and tectonic evolution history of the Tadongnan Uplift
塔东南隆起沉积-构造特征及其演化历史
12.
Structural Style and Character of Evolution for Central Uplift Belt in Qikou Depression
![点击朗读](/dictall/images/read.gif)
歧口凹陷中央隆起带构造样式及形成演化特征
13.
Tectonic Evolution of Uplift in Southeast Tarim Basin and Analysis of Their Structural Features
塔里木盆地东南隆起演化及构造特征分析
14.
Fault System and Oil-Gas Accumulation in Yaha Structural Belt of Tabei Uplift
![点击朗读](/dictall/images/read.gif)
塔北隆起牙哈构造带断裂特征与油气成藏
15.
The Structural Styles of Different Structural Layers in the Western Part of North Tarim Uplift and Their Genetic Mechanisms
塔北隆起西部不同构造层构造样式及其成因关系
16.
3、Tectonic style of the orogenic-belt uplift is very complicated,and is markedby the growing of a large number of thrusting rupture and faulted block.
3、造山隆起带构造样式较复杂,发育大量的逆冲断裂与断块体;
17.
In summary, the AVO analysis reshaped our geological understanding of the ridge as a prospect.
总之,通过AVO分析有助于我们深入理解隆起远景构造。
18.
THE GEOLOGICAL EVOLUTION FEATURESCOMPARING BETWEEN EAST ZHEJIAN UPWARPING ZONE IN CHINA AND KUROSEGAWA TECTONIC ZONE IN SOUTHWEST JAPAN
浙东隆起带与西南日本黑濑川构造带地质演化之比较