NEE and NNE fault belts controlling the formation of the basin had developed well and early and had acted for a long time.
北东东向和北北东向断层带形成较早且长期活动，控制了盆地的形成；
Cenozoic East Sag of Liaohe basin consists of double structure and is a fault depression basin with extending and strike slipping.
辽河盆地东部凹陷北段新生代盆地具下断上拗的双层结构，是伸展和走滑联合作用的断陷盆地。
The sedimentation of Tuchengzi Formation was mainly preserved in Chengde syncline and in the south part of Gubeikou fault in Chengde area, namely Chengde basin and Gubeikou basin, respectively.
承德地区土城子组的沉积地层，主要保存在两个地区，一处为承德向斜，另一处为古北口断层的南部紧邻断层地区，即分别命名的承德盆地和古北口盆地内。
The underlying volcanic fault basin combines with the overlying downwarped basin to form a basin with a binary structure.
下部的火山断陷盆地和上覆的沉积坳陷盆地组成了二元结构的盆地。
The hinge line of the basin progressively migrates towards the fault.
整个演化过程中，盆地转折线逐渐向断层移动。
Detailed analyses of satellite images and field investigation have revealed that the active Kaidu River fault zone on the southern margin of the basin is a strike-slip fault zone.
详细的卫星图像分析和野外调查表明活动断层(开都河断层带)主要分布在盆地的南缘，具典型的走滑断层特征。
Fault analysis show that Taiyuan basin is sedimentary basin of Late Cenozoic rather than rifted one.
经断裂分析，太原盆地不是裂谷盆地，而是晚新生代的沉积盆地。
Jiaolai basin is a strike-slip and pull-apart basin controlled by the Yishu Fault Belt and Wulian -jimo-muping Fault.
胶莱盆地是中生代走滑拉分盆地，其形成与发育受到沂沭断裂和五莲-即墨-牟平断裂的控制。
Two seismic fault belts with different directions in Mesoproterozoic and Neoprotertozoic control the basin boundaries of the two stages respectively.
中元古代与新元古代两个不同方向的地震断裂带分别控制着两个时期的盆地边界。
Early Jurassic to early cretaceous basin group of western Liaoning is a distinguished group of fault basin.
辽西地区的早侏罗世—早白垩世盆地群是一类颇具特色的断陷盆地群。
The small basin in the southwest of China is types of single structure halfgraben-like depression and dual structures platform-fault depression.
西南小盆地为单层结构箕状断陷型和双层（地）台、断（陷）型沉积盆地。
Shongliao basin is a rift basin with a strong fault activity and the faults in the basin are closely related to the origin and distribution of natural gas.
松辽盆地是断裂活动十分活跃的裂谷型盆地，盆内断裂与天然气的形成、分布有密切的关系。
The major sedimentary facies were alluvial fan facies and fan delta facies in the west, and stream delta and braided delta in the east, with a lacustrine facies in the centre of the fault basin.
西岸陡坡带以冲积扇和扇三角洲沉积为主，东岸缓坡带以河流三角洲、辫状三角洲占优势，盆地中心为湖相沉积。
Wuxi fault is the boundary fault of western Wuerxun depression in Hailar Basin, which plays an important role in tectonic evolution to the depression.
海拉尔盆地乌尔逊凹陷西部的边界断层—乌西断裂，对该凹陷的构造演化具有明显的控制作用。
Two phases of the structural movement lead to forming and evolution of complex fault system in the Liaohe basin.
二期构造运动导致了辽河盆地复杂断裂体系的形成和演化。
Hefei basin is a Mz-Cz residual basin generated from common action by Dabie orogen and Tanlu (TanchengLujiang) fault zone.
合肥盆地是大别造山带和郯庐断裂带共同作用产生的中新生代残留盆地。
Neotectonic activity of Yili basin shows apparent evidences on land form, fault activities and stratigraphic contact.
伊犁盆地新构造运动在地貌、断裂活动和地层接触关系等方面表现十分明显。
Methods Disscuss the basin evolvement phases according to the characteristic of the basin stratum, fault activity and depositional evolution.
方法通过盆地断裂活动特征、沉积演化特征探讨盆地演化阶段。
The characteristics of OOIP in Jiyang depression, a non marine fault basin, are very representative.
济阳坳陷是一个典型的陆相断陷湖盆，油藏特征非常具有代表性。
Shiwu fault basin is located in the southeastern margin of southeast uplift area of Songliao basin.
十屋断陷位于松辽盆地东南隆起区的东南缘。
The Yitong Graben is a Tertiary petroliferous strike-slip fault basin developed on the Hercynian fold basement.
伊通地堑是一个主体在海西期褶皱基底上发育起来的第三纪含油气走滑断陷盆地。
Hailar basin is a fault-depressed basin formed on Variscan folded basement.
海拉尔盆地是在华力西褶皱基底上形成的中生代断陷盆地。
The linear image shown by INSAR inside Fangxian basin has been proved as a hidden fault belt.
房县盆地内insar影像图上显现的线性影像证实为一条隐伏断层。
The pathway system is classified into 3 types of fault, carrier bed and unconformity in Bachu area, the Tarim Basin.
从塔里木盆地巴楚地区输导体系类型入手，将其分成断裂、输导层和不整合面等3类。
The Daqingshan Mountains and its adjacent Huhehot fault basin, Nei Monggol, are the ideal area to study denudation and uplift.
内蒙古大青山及其毗邻的呼和浩特断陷盆地是研究剥蚀和地壳均衡隆起的理想地区。
Nanpan River Basin experienced extension, fault depression in middle-late period of Early Triassic and compression fault rising after Ladinian of Middle Triassic.
南盘江盆地三叠纪，经历了早三叠世中、晚期的拉张、断陷和中三叠世拉丁期之后的挤压断隆。
Changling fault depression is a basin of continental volcanic-sedimentary rocks, faulting is the key factor that controls volcanic activities and volcanic rock distribution.
长岭断陷为陆相火山岩一沉积岩盆地，断裂运动是控制火山活动及火山岩平面分布的主要因素。
Jiaozhou Bay is a fault basin and the chess board structure has played the main control role in its formation.
胶州湾为一断陷盆地，棋盘格式构造起着主要控制作用。
Karayulgun fault located in Northern Tarim Basin is one of northwest-trending faults of Northern Tarim Basin.
喀拉玉尔滚断裂系位于塔里木盆地北部，是塔北系列北西向展布的断裂之一。
Zhaoling gold deposit lies in the east part of the joint-point of Waifangshan fault uprising and Jiuxian-Dazhang fault depression basin.
赵岭金矿床是典型的受构造控制的构造蚀变岩型金矿床，位于外方山断隆与旧县—大章断陷盆地结合部位的东部。
应用推荐