地震地层学

TX坳陷海相地层区域地震地层学研究

Seismic stratigraphy study of the marine bed in TX depression

陆相盆地中地震地层学的应用条件

The application condition of seismic stratigraphy in continental sedimentary basin , OGP

陆相断陷盆地区域地震地层学方法探讨

Regional seismic stratigraphic method for Fault-depressed basins in land

地震地层学在地层接触关系和古水流体系分析上的应用

Application of seismic stratigraphy to the study of depositional environment and paleocurrent systems

用地震地层学方法进行碳酸盐岩沉积相研究

Study of carbonatite sedimentary facies with seismic stratigraphic method

应用地震地层学解释探讨辽河西部凹陷几个地质问题

Application of seismic stratigraphy to explain some geological problems in Western Liaohe Depression

此项试验结果与地震地层学解释的结果相当吻合。

In general , this result accords with that of seismic stratigraphic interpretation .

辽东湾南部下第三系地震地层学研究

On seismic stratigraphy of Eogene in southern Liaodong Bay

地震地层学&按照地震资料解释进行地层学和沉积相的研究。

Seismic stratigraphy-the study of stratigraphy and depositional facies as interpreted from seismic data .

近代河流沉积与地震地层学解释

Recent river sediments and seismic stratigraphic interpretation

塔里木盆地三叠－侏罗系地震地层学研究

Seismic Stratigraphy of Triassic-Jurassic in Tarim Basin

塔里木盆地西南古生代地震地层学特征

Paleozoic seismic-stratigraphy of the southwestern Tarim Basin

南黄海晚第四纪地震地层学与新构造运动研究

The Studying on Late Quaternary Seismic Stratigraphy and Neotectonic Movement of the South Yellow Sea

地震地层学在沅江凹陷的应用

Application of seismic stratigraphy to Yangjiang depression

论层序地层学对地震地层学领域的发展

Advance in seismic stratigraphy & sequence stratigraphy

因此，通过生物地层学与地震地层学的综合研究，可建立层序生物地层单元，具有层序生物地层学意义；

The sequence biostratigraphic units can be established by comprehensive research of biostratigraphy and seismic stratigraphy .

美国尤金岛油田三角洲复合体的地震地层学、岩相结构和油藏特征

Seismic stratigraphy , facies architecture and reservoir character of a delta complex , Eugene island block-300 field

地震地层学在沉积学研究中的意义&从中国东部盆地下第三系地震地层及沉积学研究中得到的某些新认识四川盆地上三叠统地震地层划分对比方案

Significance of SEISMO-STRATIGRAPHY in sedimentologic study seismic-stratigraphic division and correlation project of the upper Triassic System in Sichuan Basin

继地震地层学、层序地层学之后，又出现了一门新的边缘交叉学科&地震沉积学。

Following seismic stratigraphy and sequence stratigraphy , there has been a new emerged edge inter-discipline & seismic sedimentology .

层序地层学是在地震地层学基础上发展起来的新的地学分支学科，为沉积地质学与地球物理学架设了新的桥梁。

Sequence stratigraphy is one of the subject which has been recently developed on the basis of the seismic stratigraphy .

歧口凹陷凹槽区利用地震地层学解释技术研究砂体分布。

The distribution of sands in the trough zone of the depression is studied by using seismic stratigraphic interpretation method .

运用地震地层学方法，在笔架南盆地识别出5个特征明显的反射界面，划分了3个超层序、5个地震层序，并探讨各地震层序的地质时代。

From seismic stratigraphy , the authors identify five seismic reflection interfaces and differentiate five seismic sequences and three supersequences .

地震地层学自其问世以来，在油气勘探的实际应用中不断地得到发展和完善。

Seismic stratigraphy has been developed and improved continuously in practical application in oil and gas exploration since it came out .

地层岩性油气藏是苏北盆地寻找新生代非构造圈闭油气藏的一种重要类型。文章利用地震地层学的概念，对苏北陆相沉积盆地的新生代地层作了初步应用。

Stratigraphic and lithologic oil and gas reservoirs are the chief non-structural trap of this type in the Cenozoics of the North Jiangsu Basin .

油气层序地层学是在地震地层学、层序地层学、石油地质学基础上发展起来的一门综合性新型边缘学科。

Oil / gas sequence stratigraphy is a new comprehensive borderline subject developed on the basis of seismic stratigraphy , sequence stratigraphy and petroleum geology .

作者针对河流相地层的特点，用大量薄层反射的正演模型，对每个问题作了探讨，以便促使陆相沉积地层的地震地层学取得更深入的发展。

By forward modelling the reflections of thin channel layers , the author approached the problems so as to promote tbe development of seismic stratigraphy of continental formation .

以地震地层学理论为指导，通过模型正演，建立了储层强波峰、强波谷含气砂体地震响应特征，在此基础上，进一步运用地震属性分析预测储层的平面分布。

By means of seismic stratigraphy and forward modeling , set up the " strough peak and trough " seismic response model of rhe gas-bearing sandstone and predict the gas bearing sandstone .

在东海陆架区应用地震地层学方法进行了地震层序划分及地震相与沉积环境的解释。

In the continental shelf area of China 's East Sea , the division of seismic sequence and the interpretation of seismic phase and sedimentary environment have been performed using seismic stratigraphy .

作为区域地震地层学研究的核心内容，地震相解释即沉积相恢复具有数据量大、控制因素多和解释结果不唯一等多种不利因素；

Seismic facies interpretation ( sedimentary facies recovery ) which is the essential of areal seismic stratigraphy involves some troubles : big data volume , many control factors , ambiguous interpretations and so on .

由于河流相层序地层成因和相构成的复杂性，以被动大陆边缘地震地层学研究为基础、以三分体系域构成为地层预测模式的经典层序地层学分析方法并不一定适合河流相储层。

Sequence stratigraphy conventional sequence stratigraphy interpretation techniques based on seismic stratigraphy in passive continental margin is generally considered difficult to be applied to fluvial facies due to the sequence complexity and multiple mixed facies .