泌阳断陷陆相层序外部构型研究包括层序级别的厘定与划分以及界面的类型及其识别标志。
The study on the outer configuration of terrigenous sequence in Biyang fault depression includes sequence classification and boundary identification.
本文全面总结了露头层序、测井层序及地震层序层序划分、层序界面、沉积体系和体系域的识别方法。
In this paper, The division of sequence in outcrop, log well and seismic and sequence interface and depositional system and system track was detailed discussed.
层序界面和层序内体系域的识别除宏观的沉积记录分析方法外，还可通过微观的沉积地球化学分析资料来识别。
Besides the macroscopic sedimentary records analytical methods, the sequence boundary and inter systems tract can also be identified by microcosmic analysis information of sedimentary geochemistry.
重点进行了高分辨率层序界面的识别和对比、高分辨率层序地层划分和内部单元构成分析、基准面旋回识别和对比。
The emphasis of this paper is to identify, contrast and divide the high-resolution sequence interface, analyze the constitution of its internal units, identify and contrast the base level cycle.
根据关键界面识别，苏南地区三叠纪地层可划分为3个层序。
The Traissic Stratigraphy in South Jiangsu can be classified into 3 sequences based on the distinguishment of crucial interface.
层序地层分析的关键在于不同级别层序界面的识别，准层序是测井层序地层分析的最小基本单元。
The key of sequence stratigraphy analysis lies in recognizing sequence boundaries of different levels. Parasequence is the minimum unit of sequence stratigraphy analysis of well-logging.
层序地层分析的关键在于不同级别层序界面的识别，准层序是测井层序地层分析的最小基本单元。
The key of sequence stratigraphy analysis lies in recognizing sequence boundaries of different levels. Parasequence is the minimum unit of sequence stratigraphy analysis of well-logging.
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