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On the basis of varied-direction seismic data ( including 3-D seismic data) from the downthrown side of the southern ZH fracture, an anomaly volume with large thickness and wide range, which is different from the surrounding seismic facies has been found on the Paleogene strata.

本文依据ZH地区A-2构造南断裂下降盘多个方向的地震资料(包括三维地震资料),发现在下第三系地层里存在一个厚度大,范围广,与周围地震相截然不同的异常体。

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Seismic Facies And Trap Types of Igneous Rocks in TZ Area, Tarim Basin

塔中地区火成岩的地震相及圈闭特征

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based on the principle of seismic stratigraphy, eight kinds of seismic facies unit are identified in kong2 member.

运用地震地层学原理,在孔二段中识别出八种地震相单元。

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expert system for seismic facies interpretation in continental fault basin

陆相断陷盆地地震相解释专家系统

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seismic facies analysis of group j3 in t depression of s basin in the western china

西部S盆地T凹陷J3组地震相分析

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miocene seismic velocity facies in ruili basin, western yunnan

滇西瑞丽盆地中新统地震-速度相

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use of synthetic vsp logging data and seismic records to establish log sequence and the relationship between seismic sequence analysis sedimentary environment, the establishment of sedimentary facies pattern, distribution of depositional systems derived features.

利用VSP测井资料及地震合成记录建立测井层序与地震层序之间的关系,分析沉积环境,建立沉积相模式,得出沉积体系展布特征。

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

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。

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Based on seismic, well logging, borehole log and core data, applying principles and methods of tectonics, sedimentology and seismic stratigraphy, tectono-sedimentary evolution of Tangyuan Rift and sedimentary facies are studied.

以地震、测井、录井和岩心资料为基础,应用构造学、沉积学和地震地层学原理和方法,对汤原断陷的构造沉积演化和沉积相进行了研究。

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Reflective Seismic Simulation on the China terrestrial facies fault depression model

中国反射地震陆相断陷模型简介

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Analysis on the characters of seismic reflection, gravity filed, interval velocity, rock's density, tectonic features of depression, well_to_well interpretation and sedimentary facies of surroundings proved that Mesozoic marine strata are widespread in the eastern area of Pearl River Mouth basin.

从地震反射特征、重力场特征、层速度特征、岩石密度特征、坳陷构造形态特征、连井解释以及区域沉积相的研究,多个方面阐明了在珠江口盆地东部地区广泛存在中生代海相地层。

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Finally, according to a thin rock section analysis in the laboratory, sedimentary facies analysis, logging data analysis and the reef-complex seismic data interpretation, the authors think that the seismic abnormity is effected by the Carbonic-Devonian organic reef clusters.

然后,通过实验室薄片分析、沉积相分析、测井研究、礁复合体的地震解释等研究工作,最终认为其地震异常为石炭-泥盆系生物礁群的反映。

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Combined with seismic data, the main volcanic facies are explosive facies, effusive facies and volcanic sedimentary facies.

结合地震资料,其火山岩岩相主要为爆发相、溢流相、火山沉积相。

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The facies has large depositional thickness, showing colina shape, desultory interior reflections and extension along major structural alignment on seismic section.

该相沉积厚度相对较大,在地震剖面上反映为丘状隆起,内部反射杂乱,呈乱岗状反射,多沿主要构造线延伸。

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