Discovery of late-Paleozoic syndepositional faults in Hexi area;
贺西地区晚古生代早中期同沉积断层的发现及其意义
At last,it studied the double actions of the syndepositional faults and their seco.
文章系统总结了同沉积构造的发育机理、影响因素,综合分析了同沉积构造对烃源岩、储集体和含油气圈闭的控制作用,并研究了同沉积断层及其次生断层在油气运移和聚集过程中的双重作用。
The east inclined synsedimentary fault and oil -gas accumulation in Dongpu sag.;
东濮凹陷东倾同沉积断层与油气聚集
Two kinds of slope-breaks are developed in this basin, one is the syndepositional fault slope-break, the other is the syndepositional bend slope-break, whic.
根据古构造坡折带控制层序类型和层序构成模式的思路 ,通过南堡凹陷古近系同沉积构造发育特征的分析 ,认为南堡凹陷古近系存在同沉积断裂坡折带和同沉积背斜挠曲坡折带 2种类型 ,由此决定了南堡凹陷古近系主要发育了同生断裂坡折型层序和同沉积背斜挠曲坡折型层序 ,建立了这 2种类型层序体系域构成模式 。
The controls of the syndepositional faults are manifested in:(1) the controls of the active basin-margin faults in the steep slope zone on the distribution of the fan delta facies;(2) the controls of the active basin-margin faults in the ramp zone on the distribution of the braided delta facies;(3) the c.
同沉积断裂特征对沉积具有控制作用,陡坡带活动盆缘断裂控制扇三角洲的分布,缓坡带活动盆缘断裂控制辫状河三角洲分布;二级断裂对湖底扇和深水沉积区有明显的控制作用,东部断阶带中部发育的F20东西向同沉积断裂,控制了物源的主要注入通道——沟谷,对东部物源的注入具有长期影响。
The study proved that horizontal migration of platform margin was mainly controlled by syndepositional faults,the vertical sequence evolution of platform margin was mainly controlled by sea-level change,the type of margin reef-bank was controlled by different types of carbonate secret organisms.
这4个阶段的台缘沉积特征表明:台地边缘礁滩沉积体系垂向演化受海平面变化控制,横向迁移主要受同沉积断裂控制,不同类型生物的出现和绝灭控制台缘生物礁滩的类型及特征。
The petrological and petrochemical characteristics indicate that the formation of these conglomerates was controlled by synsedimentary faults during the metallogenic e.
通过对该类砾岩岩石学和岩石化学研究 ,认为其形成受控于成矿期的同沉积断裂。
Characteristics and exploration significance of the hydrocarbon migration system controlled by the synsedimentary reverse faults in the southwest area of Qaidam Basin
柴达木盆地西部南区同沉积逆断层控制下的输导系统特征及其勘探意义
Fault ptures would generally be absorbed by unconsolidated deposits.
断层破裂一般会被未固结的沉积物所吸收。
DEVELOPMENT OF THE FAULTS AND ITS CONTROLLING TO THE DEPOSITION IN THE EAST AREA OF LINQING DEPRESSION
临清拗陷东部断层发育及其对沉积的控制作用
Syndepositional structural slope-break zone is a basic characteristic of rift-subsidence basin.
发育同沉积构造坡折带是断陷盆地的基本特征。
The Research on Sequence Stratigraphy and Sedimentary Facies of the Member 4 of Yingcheng Formation in Xujiaweizi Depression
徐家围子断陷白垩系营城组四段层序地层及沉积相
folding and thrusting
褶皱和逆掩断层作用
The strike-slip-thrust fault strikes to 280-305°and the fault plane dips to southwest with angle of about 30°.
走滑逆断层走向为280°—305°。
a sedimentary rock formed by the deposition of successive layers of clay.
一种由粘土逐层沉积而成的沉积岩。
Depositional System Distribution Characteristics in Sequene Stratigraphic Framework of Tangyuan Fault Basin and Sequence Stratigraphic Models Establishment;
汤原断陷始新统层序地层格架内沉积体系分布特征及层序地层模式的建立
Time and Space Distribution of Depositional System and Reservoir Research for the Forth Member of Shahejie Formation of Shang 25 Fault Block in Huimin Sag;
惠民凹陷商25断块沙四段沉积体系时空展布与储层特征研究
Research of the Structural Evolution and Its Sedimental Response in Changling, Shiwu Faulted Depression of the Sourthern Songliao Basin
松辽盆地南部长岭、十屋断陷层构造演化与沉积响应研究
Study on Huoshiling Stage-Yingcheng Stage sedimentary micro-facies and reservoir recognition in Shiwu fault depression.
十屋断陷火石岭组—营城组沉积微相研究与储层识别
overthrust nappe
【地质】逆冲体, 逆掩断层推覆体
cermet electrodeposited coating
陶瓷金属电沉积涂层
Sediments acted as a restricting control.
沉积层起着屏蔽的作用。
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。
A deposit, as of ore, parallel to local stratification.
沉积物平行于局部地层的沉积物，如矿层
DEVONIAN SYNGENETIC FAULTS AND LITHOFACIES IN RELATION TO SUBMARINE EXHALATIVE SEDIMENTARY LEAD-ZINC DEPOSITS IN QINLING AREA, SHAANXI PROVINCE
陕西秦岭地区泥盆系同生断裂、岩相与海底喷流沉积铅锌矿床