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1)  sedimentary facies sequence
沉积相序
1.
The authors hold that the transform surface of stratigraphic accumulation type and disconnected surface of sedimentary facies sequence are indirect marks of sequence boundary.
认为地层堆积类型转换面及沉积相序向上突然变浅的间断面是层序界面的间接标志。
2)  sequence-facies model
层序-沉积相模式
3)  nonmarine depositional sequence
非海相沉积层序
4)  depositional sequence
沉积层序
1.
It is found that the passage systems of different sequences have difference:(1) The passage systems of deep depositional sequences(Ek-Es4)are characterized by the complex hydrocarbon conduction in the sides of sandbodies.
针对东营凹陷的地质特征,利用输导体系综合研究方法,分析了盆地输导体系的构成,发现东营凹陷不同沉积层序在输导体系结构特征上存在差异性:①深部沉积层序(Ek-Es4)输导特征主要表现为砂体侧向复式输导。
2.
These Cambrian strata have been grouped, on the basis of sedimentary facies sequences and stacking patterns of depositional sequences, into 63 third order sequences, or 22 second order megasequences and 4 first order supersequences, of which the latest ones represent the depositional cycles with the periods of 200-400 Ma during 1800.
以岩相及相序为基础 ,不同级别沉积层序及其有序叠加形式为研究核心 ,在这套厚度巨大的前寒武纪地层中识别出 63个三级层序 ,可进一步划归为 2 2个二级大层序 ,4个一级超层序。
3.
Based on the theory of continental foreland basin combining with petroleum exploration practices,Basijiqike formation reservoir of Cretaceous in Kuqa foreland basin controled by continental depositional sequence has been studied.
文中紧密结合生产勘探实践 ,充分运用陆相前陆盆地的观点对库车前陆盆地陆相沉积层序控制下的白垩纪巴什基奇克组储层进行了重点研究。
5)  depositional sequence
沉积序列
1.
Based on the bore section, combining with the study on lithology, well logging, seismic facies and sequence type, the structure of the sequence in the deeply down-faulted Dongying Sag is analyzed emphasizing on the low-stand fan depositional type, its controlling factors and depositional sequence.
以钻井剖面相分析资料为基础,结合岩性、测井、地震响应特征及层序类型分析,研究东营凹陷深陷期层序的构成,着重探讨其中低位扇的沉积相类型、发育的控制因素及沉积序列。
2.
On the basis of an analysis of the characteristics of Quaternary depositional sequences and sporopollen assemblages in the Gonghe basin,combined with the thermoluminescent dating,the authors have studied the environmental change in the basin since the Quaternary and divided the change into two major phases:the early .
通过对共和盆地第四系沉积序列特征和孢粉组合特征的分析,结合热释光测年,本文较详细地研究了共和盆地第四纪以来的环境变迁,并将其分为两大阶段:早期为湖相沉积阶段(中更新世晚期~0 079Ma),气候相对温和。
3.
It can be divided into 3 depositional sequences(succession of strata), i.
可划分为三个沉积序列(层序)。
6)  sedimentary sequence
沉积层序
1.
Hydrocarbon evaluation analysis is based on different level research, such as basin analysis, sedimentary sequence analysis, and petroleum system analysis.
油气盆地、沉积层序与油气系统的研究属于不同层次的油气资源评价的基础研究。
2.
An investigation of sequence stratigraphy shows the Jurassic system in Kuqa Depression of Tarin basin can be divided into 8 sedimentary sequences, of which type I sequence boundary dominates.
通过层序地层学的划分与对比 ,将侏罗系划分出 8个沉积层序 ,层序界面以I型层序界面为主。
3.
By means of the research method of sedimentary geology, it is studied in detail on the petrologic characteristics, sedimentary sequences and distribution of the coal bearing strata below seam No 15, Taiyuan Formation in the Wuda Mine District, Neimenggu Autonomous Region, China.
用沉积地质学的研究方法对内蒙古乌达矿区晚古生代太原组15号煤层下含煤岩系的岩石学特征、沉积层序和展布格局进行了详细研究,认为15号煤层堆积于潮下砂坪沉积环境。
补充资料:相序
1.依次。
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