1.
Structural Features and Fault Quantitative Study in Donghuantuo Coalmine
东欢坨矿构造特征及断裂构造定量研究
2.
Fracture Structure of Cretaceous Red Basin of “Forest Stop”in Mid Wujiang River
乌江中游“森林站”白垩系红盆断裂构造
3.
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
4.
Structural Characteristic and Seal Evaluation of Fault in the North of Chaidamu Basin;
柴北缘断裂构造特征及其封闭性评价
5.
Analysis and Prediction of Characteristics of Fracture Structure in Xinwen Coalfield
新汶煤田断裂构造特征分析及其预测
6.
Geochemistry Characteristics of Faulted Structure in Dushan Banian Antimony Deposit
独山巴年锑矿断裂构造地球化学特征
7.
Study on lithologic reservoir of Baoriwendu faulted structure belt in Luxi sag
陆西凹陷包日温都断裂构造带岩性油藏研究
8.
The Effect of Fractures on Rock Stresses and Its Significance in Geological Engineering;
断裂构造对地应力场的影响及其工程意义
9.
Study of the Bolting Technique about Entry of Deep Shaft's Fracture Zones;
断裂构造区域深井回采巷道锚杆支护技术研究
10.
Neotectonics and neotectonic activities of Yingkou-Weifang fault zone
营口—潍坊断裂带的新构造和新构造活动
11.
According to the researchresult, the tectonite consists of mylonite and cataclasite in the fracture zone.
断裂带的构造岩以糜棱岩和碎裂岩为主。
12.
Study on the Tectonic Stress Fields of Meso-Cenozoic Era of Jinhuo Fracture Zone
晋获断裂带中、新生代构造应力场研究
13.
The Study on Characteristics of Structural Deformation of the Nenjiang-Balihan Fault Belt in Northeastern China;
嫩江—八里罕断裂带构造变形特征研究
14.
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
15.
STUDY OF STRUCTURAL CHARACTERISTICS OF XIANGFAN-GUANGJI FAULT IN HUBEI PROVINCE
襄樊—广济断裂湖北段构造特征研究
16.
Classification of Faults in the Zhongwei Fault Zone and Its Tectonic Implication
中卫断裂带断层类型划分及其构造意义
17.
The backbone fault is the Litianmu Fault and Zao2301 Fault taking to NE,controlling the formation of sedimentary and structure of studing area.
其中北东向李天木断裂和枣2301断裂是主干断裂,控制研究区地层沉积和构造形成。
18.
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;