根据最新的三维地震解释成果和钻探资料，分析了松辽盆地南部长岭凹陷腰英台区块断裂构造特征。
On according the newest three earthquake preserve explaining fruit and drilling data of South Songliao basin in Yaoyingtai Changling sag area, analysis the rupture structure character.
[4]赵希刚。鄂尔多斯盆地不同沉积地层中的断裂构造特征识别[J]。中国核科技报告，2006 (1)：191- 199。
ZHAO Xi-gang. Signature Recognition for Rift Structures of Different Sediment Strata in Ordos Basin [J]. China Nuclear Science and Technology Report, 2006 (1) : 191-199.
三山岛金矿区位于胶东半岛西北部，区内构造、岩浆活动强烈，以发育脆性断裂为特征。
Sanshandao gold mine is located in the northwest of Shandong peninsula, structure and magmatic activity of this area are strong, and it is characterized by development of brittle fracture.
掌握断裂构造对地下水的控制特征。对于分析和寻找地下水资源，无疑是有意义的。
To know well the water controlling features of faulted structures is meaningful in analyses and finding of groundwater resources.
然后分析区域构造特征和展布格局，特别强调逆冲推覆断裂的重要性；
Then, the regional structure characteristics and distribution pattern are analyzed and the importance of thrust nappe fault is emphasized especially.
依据地质资料，讨论了平庄盆地NNE—EW向断裂构造对地下水的控制特征。
According to geological data, the paper discussed groundwater-controlling features of NNE and EW faulted structures in Pingzhuang basin.
康滇菱形块体的边界断裂具有不同的密度特征，显示出不同的构造性质。
The boundary faults of Kangdian block are of different density features, suggesting different tectonic signification.
在地表地质调查并结合钻井资料分析的基础上，主要通过地震剖面的精细地质解释，对阿尔金断裂东段的构造变形特征进行了系统分析。
Based on the seismic profile interpretation as well as ground survey and well data, the paper presented structural deformation features of the eastern sector of Altun fault.
断裂构造往往具有多期叠加变形的特征。
The fault structures often have a characteristic of multiple phases and superimposed deformation.
盐源菱块边界断裂的几何形态决定了这一地区现代构造应力场的基本特征。
Geometric pattern of the border faults around the Yanyuan rhombic block has defined the basic features of the contemporary tectonic stress field in that region.
断裂和断块构造是南海北部陆缘新生代构造作用的基本特征。
Structures of faults and fault-blocks are the basic characteristics of tectonism in the north continental margin of South China Sea in the Cenozoic.
利用相干体技术研究断层、微断裂的空间分布、地质构造异常及岩性的整体空间展布特征。
Use coherence technology to research the spatial distribution of fault and micro-fracture, the abnormal of geological structure and characteristics of the spatial distribution of lithology.
构造地貌能反映断裂的结构变形特征和断层的活动强度。例如断层陡坎的高度、长度和坡度以及断层陡坎的连续程度。
Tectonic topography can reflect the structural deformation feature and active strength of faults, such as the height, length and gradient of a fault scarp as well as its continuity.
运用三维地震资料、精细地震解释，结合钻井资料进行构造研究，分析描述该区的构造特性、断裂特征。
Applying three-dimensional seismic data and seismic explanation, on the basis of drilling data, we analyze and describe the structural feature and fracture feature.
本文通过对该区区域地震资料的研究，分析断裂和局部构造的特征、性质、成因机制和分布范围，阐述西湖凹陷的演化历史。
This paper analysis feature, property, cause of formation and distribute of failure and local structure and expound basinal evolution in Xihu Trough.
在云龙锡矿带内，断裂构造分级控岩、控矿的特征是极为明显的。
The characteristics of the grading control of diagenesis and metallogenesis by the fracture structures in the tin-ore belt of Yunlong is very obvious.
区域勘探确定了盆地基底南北分区特征，它对盆地的断裂展布、构造发育具有严格的控制作用。
Regional exploration has revealed that the basin basement is divided into southern and northern parts, and this plays a strictly controlling role in the fault distribution and structure development.
结合该区已知的地质构造特征综合分析，重力负值带是早元古宙拗拉槽边界深断裂和构造—岩浆岩带的反映。
Considering the known synthetical studies on the characteristics of geological structures, the negative gravitational belt is considered to be a deep fracture or a tectonicmagmatic belts.
对剖面中反映的构造反转、褶皱组合样式、逆冲断裂带、直立地层发育带的构造特征进行了探讨。
Structural characteristics of inversion structure, fold association style, thrust fault zone upright strata developed belt shown in great profiles were also discussed.
控矿构造主要为NNE向断裂，具明显的双重结构面特征，金矿体严格受其控制。
The ore controlling structure is mainly NNE strike fault with double constructional surface.
本文根据近年来野外考察的实际资料，总结了右江断裂带的新构造活动特征。
Based on the practical data from field survey in recent years, this paper makes a summary on neotectonic characteristics of Youjiang active fault zone.
利用断裂带的共轭节理、断面擦痕和阶步及显微构造反演恩施断裂3个主要变形期的运动学和动力学特征。
The kinematic and dynamic features of the Enshi fault in the 3 main deformational phases are analyzed by means of the striations on fault planes, conjugate joints and microstructure in fault zone.
论述了川西甘孜—理塘断裂带构造演化与金矿床成矿作用的关系，总结了区内金矿化的特征和金矿床类型。
The tectonic evolution of Garze Litang fracture zone, the characteristics of gold mineralization and types of gold deposit as well as their relationship in west Sichuan are expounded in this paper.
构造岩透射电镜分析结果进一步证实了该断裂的存在并具深断裂的特征。
The result of TEM analysis of mylonites of the Guandian-Longwangjian fault has verified the existence of this fault and revealed its deep-fault features.
各段断裂结构、伴生构造、褶皱组合样式、岩石变形等构造特征存在一定差异。
There are some differences among these sections in structure characteristic, such as fault structure, associated structure, fold association style, deformation of rock, and so on.
煤田中部地质构造相对简单，控煤构造样式以褶皱-断裂型为特征，含煤岩系赋存稳定，是有利的勘查开发区段。
Structures in middle zonation are simple and coal-controlled structural style is characterized by fold-thrust pattern, coal measures distributed stable in favor of exploration and development.
浙江萤石矿严格受断裂构造控制，构造控矿特征明显。
The fluorite deposits are controlled strictly by faults in Zhejiang Province. The characteristics of structural ore-control is very obvious.
本文首先从郯庐断裂与渤海盆地的关系入手，分析郯庐断裂与渤海湾盆地的关系及郯庐断裂在渤中地区的构造特征。
This paper studies the relationship between the TLF and Bohai basin and the structure character of TLF in Bozhong sag.
本文首先从郯庐断裂与渤海盆地的关系入手，分析郯庐断裂与渤海湾盆地的关系及郯庐断裂在渤中地区的构造特征。
This paper studies the relationship between the TLF and Bohai basin and the structure character of TLF in Bozhong sag.
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