1) structure sequence interface
构造层序界面
1.
Division of the structure sequence interface of middle-shallow layer in Songliao basin and its effect on the petroliferous system formation;
松辽盆地中浅层构造层序界面的划分及其对含油气系统形成的意义
2) sequence boundary
层序界面
1.
Relationship between hydrocarbon reservoir and genetic types of sequence boundary in rift lacustrine basin;
断陷湖盆层序界面的成因类型及其与油气藏的关系
2.
Identification method of sequence boundary for Eogene of Chengbei step-fault zone in Dagang offshore area;
大港滩海区埕北断阶带古近系层序界面的识别方法
3.
Response characteristics of sequence boundary in geophysical data.;
层序界面在地球物理资料上的响应特征
3) sequence interface
层序界面
1.
According to the genetic sequence interfaces and regional tectonic movement,Tertiary strata in Nanpu depression can be divided into 7 super-sequences,missing only the 2nd super-sequence by comparison with other basins in Bohai Gulf.
南堡凹陷第三系依成因层序界面及区域构造活动 ,可划分出 7个超层序 ,与渤海湾其他盆地相比 ,仅缺失第 2超层序。
2.
In analysis of imaging stratigraphy for Cretaceous terrestrial basin in Xingjiang,in the light of modern stratigraphic theory,using analysis methods of sequence stratigraphy and tectonic sequence,the recognition marks of imaging sequence interfaces in remote sensing are built, and combined with 1∶50000 geological survey,the interpretating methods of imaging tectonic sequenc are discussed.
在信江白垩纪陆相盆地的影像地层分析中，以现代地层学理论为指导，运用层序地层和构造层序分析方法，建立了遥感影像层序界面识别标志，结合１∶５万地质填图，论述了影像构造层序的解译方法。
3.
Through analyzing field profiles in Ningzhen area of Jiangsu, characteristics of 4 key genesis types of Lower Palaeozoic sequence interface are analyzed in the area, classification of the Lower Palaeozoic sequence stratigraphy is made, of which 5 second stage sequences and 34 third stage sequences are established.
通过江苏宁镇地区的野外剖面研究,分析了该区下古生界四种主要成因类型的层序界面特征,对该区下古生界地层进行了层序划分,共划分出5个二级层序、34个三级层序。
4) Structural interface
构造界面
5) structural sequence
构造层序
1.
Two kinds of revolutionary models for sequences including structural sequence model and climate sequence model developed in foreland basin were presented.
研究结果表明,前陆盆地内发育有两种层序模式,即构造层序和气候层序。
2.
The structural sequences of stretch rift basin is usually composed of coarse grain sequence in the bottom,volcanic rock bearing sequence in the lower part,deep water sequence in the mid part and filling sequence in the upper part.
伸展裂谷型盆地的构造层序由下而上一般由底部粗粒层序组、下部含火山岩层序组、中部深水层序组和上部充填层序组组成 ,南堡凹陷据此可划分出 6个构造层序 ,其中第三、四构造层序控制了南堡凹陷两期主要的含油气系统分布。
3.
Integrated information about geology, geophysical and assaying, study structural sequence and sedimentary system of transition period of fault sag in Jiyang depression.
运用地质、地球物理和分析化验等综合资料,对济阳坳陷的断-拗转型阶段的构造层序及沉积体系作了系统的研究。
6) tectonic sequence
构造层序
1.
A study on Paleogene tectonic sequences in Bozhong sag;
渤中凹陷古近系构造层序研究
2.
The structural features and their controlling action over the sedimetation in the area were studied, and the sequence boundaries within the basin were traced and correlated using the tectonic sequence analysis method.
应用构造层序分析方法 ,研究了区内的构造特征及其对沉积的控制作用 ,对盆地内层序界面或区域性层序界面进行了追踪对比 。
3.
Through comparing the tectonic sequences stratum of Triassic-Paleogene period in the east of Hubei,in Jingmen-Dangyang basin,in Zigui basin and in the northeast of Sichuan,on the southern margin of the eastern Qinling and Dabie orogenic belt,three main tectonic sequences are divided.
通过对东秦岭-大别山造山带南缘鄂东地区、荆当盆地、秭归盆地和川东北地区三叠纪-古近纪的构造层序对比研究,划分出三个大的构造层序,并分析了中上扬子地区印支期以来沉积盆地性质转换和迁移过程与构造层序的耦合关系,揭示了东秦岭-大别造山与成盆作用过程。
补充资料：构造层
一定大地构造单元里在一定构造阶段中形成的具有特征性的构造- 地层组合。一个构造层包括一套有代表性的某些沉积建造组合或沉积-火山建造组合,在构造上具有典型的褶皱-断裂组合形式,而且常伴有特征性的岩浆岩系列。各构造层之间的分界通常是角度不整合或平行不整合（见不整合）。
大的构造层，可分为若干亚构造层，代表大的构造演化阶段中某一较小的构造演化阶段形成的构造- 地层组合。如一级大地构造单元地台和地槽有相应的地台构造层和地槽构造层。地台构造层又分为基底或变质基底构造层和盖层构造层，盖层构造层还包括一些亚构造层，例如中国华北地台的盖层构造层可分为中上元古界- 下古生界（亚）构造层、上古生界- 三叠系（亚）构造层等。
对构造层中沉积建造、构造形式和岩浆活动的研究，有助于确定研究地区大地构造属性及其演化。构造层中构造的样式、方位和强度是分析构造作用性质和构造应力场的基本依据。根据地层组合中各种岩石建造及其厚度和变化，可以恢复各时期的古地理以及升降运动的强度、幅度和差异性。
大的构造层，可分为若干亚构造层，代表大的构造演化阶段中某一较小的构造演化阶段形成的构造- 地层组合。如一级大地构造单元地台和地槽有相应的地台构造层和地槽构造层。地台构造层又分为基底或变质基底构造层和盖层构造层，盖层构造层还包括一些亚构造层，例如中国华北地台的盖层构造层可分为中上元古界- 下古生界（亚）构造层、上古生界- 三叠系（亚）构造层等。
对构造层中沉积建造、构造形式和岩浆活动的研究，有助于确定研究地区大地构造属性及其演化。构造层中构造的样式、方位和强度是分析构造作用性质和构造应力场的基本依据。根据地层组合中各种岩石建造及其厚度和变化，可以恢复各时期的古地理以及升降运动的强度、幅度和差异性。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条