• The sedimentary evolution and paleostructure in the western Qaidam Basin were discussed by combining dynamic and whole states.

    利用动态联系与整体相结合的思路,分析了柴达木盆地西部地区沉积演化和古构造特征,确定了该地区主要成藏期。

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  • Tectono -sedimentary evolution of the basin may be divided into three stages: continental margin rift, back-arc rift, and depression basin.

    其沉积—构造演化可划分为三个阶段:大陆边缘裂谷、弧后裂谷和拗陷盆地。

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  • Tectono - sedimentary evolution of the basin may be divided into three stages: continental margin rift, back-arc rift, and depression basin.

    其沉积—构造演化可划分为三个阶段:大陆边缘裂谷、后裂谷和拗陷盆地。

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  • Through the base deposition maps, the analysis of sedimentary environment, defined the Xishanyao formation's characteristics of sedimentary evolution.

    通过沉积基础图件、沉积环境的分析明确了研究区西山窑组沉积演化特征。

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  • At last, according to the palaeogeography characteristic and sedimentary evolution model, the general sedimentary facies model of Jurassic in Qiangtang basin was founded.

    根据羌塘盆地侏罗系古地理特征及沉积演化模式,建立了适合于本区的侏罗系综合沉积模式。

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  • A generalized sedimentary-tectonic model for extensional coal basin is presented, together with the explanation for the evolution of basin architecture and the conditions of peat accumulation.

    本文提出了拉伸煤盆地最一般的沉积—构造模式,并用以解释盆地结构的演化和泥炭聚积的条件。

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  • Sedimentary environment and tectonic movement have great influence on abundance and thermal evolution extent of organic matters.

    沉积环境和构造运动对有机质丰度和热演化程度影响较大。

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  • The tectonic subsidence analysis and dynamic mechanism of the basin evolution are processed in the main sedimentary basins across this belt.

    并对组成喜马拉雅造山带各种主要沉积盆地进行了构造沉降分析,研究盆地演化动力机制;

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  • The paper deals systematically with the formative conditions, sedimentary processes and model evolution of Lasaxin delta in Songliao Basin.

    本文对喇萨杏主力三角洲的形成条件、沉积过程和模式演变进行了较系统的研究。

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  • The coupling relationships between sedimentary basins and orogenic belts refer to all of their interactions in their formation and evolution.

    盘山系统形成演化过程中造山带和沉积盆地之间一切相互作用的总和即为盆山间的耦合关系。

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  • The classification of strata has a great effect on the knowledge about structural evolution, sedimentary environment and even evaluation of hydrocarbon potential in a basin.

    地层是一切地质问题的基础,地层的划分直接影响着对盆地构造演化、沉积环境甚至对全盆地含油气远景的认识。

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  • The sedimentary fillings of Qianjiang Formation are mainly controlled by structural evolution and ancient climate conditions.

    潜江组沉积充填主要受到盆地的构造演化和古气候条件控制。

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  • Being the outside strand of Hangzhou Bay, Chuanshan peninsula is very complex in such aspects as dynamic condition, sediment transport, sedimentary process and morphological evolution.

    穿山半岛北侧是杭州湾的外海滨部分,其水动力条件、泥沙运移、沉积过程和地貌演变复杂。

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  • Along the continental margin in East China Sea, the origin and evolution of Tertiary sedimentary basins are discussed, based on analyses of basement nature.

    根据基底性质分析,探讨了东海大陆边缘新生代沉积盆地的形成演化与成因机制。

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  • On the basis of sequence frame, combined with growing characteristics and lithologic feature of Beir depression, stratigraphic sedimentary pattern of different evolution stage are obtained.

    在建立层序地层格架的基础上,结合盆地的演化特征及岩性变化,做出了本区不同演化阶段的沉积模式图。

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  • The characteristic of basin's evolution affects the structure of the sedimentary formation directly.

    盆地演化的特征直接影响盆地沉积建造的结构特征。

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  • On the basis of macro depositional setting, micro sedimentary features and evolution regularity of sedimentary facies, sedimentary patterns of the research area have been established.

    在综合考虑宏观沉积背景及微观沉积特征的基础上,根据沉积相的演化规律,建立了研究区沉积模式。

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  • Sedimentary facies division and paleogeographic evolution of gas-bearing intervals in lower Permian in northern Ordos basin.

    鄂北下二叠统含气层段沉积相划分及古地理演化。

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  • This new explanation has provided new evidences for the interpretation of the nature and evolution of the Devonian sedimentary basins in the Longmen Mountain area.

    认为区内早埃姆斯期属深水陆棚至深水盆地沉积环境,为龙门山区泥盆纪沉积盆地的性质和演化提供了新资料。

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  • The evolution of sedimentary environment in the Quaternary in Dongting Basin is analyzed by using the flow energy index.

    利用水流能量指数,分析了洞庭盆地第四纪沉积环境的演变特征。

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  • This paper discusses the geometrical style, formation and evolution of deformed structures in the large scale Meso Cenozoic sedimentary basins in the west of China.

    重点讨论了中国西部中新生代大型沉积盆地变形构造的几何结构样式、形成与演化模式。

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  • The correlative relationship between increment of subaquatic accommodation space and synchronous sedimentary volume controlled the evolution of sequence and the formation of system tracts.

    水下可容空间增量与同期供给的沉积物体积之间的对比关系控制层序的演化和体系域的形成。

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  • The stratigraphic sequences in foreland basins have recorded a long and complex history of polycyclic sedimentary tectonic evolution.

    前陆盆地地层的层序反映了前陆盆地构造演化史为一个多旋回的沉积构造演化史。

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  • The evolution features of the Jiaolai Basin are discussed in this paper on the basis of its regional structure, geodynamic background and sedimentary features of the Mesozoic and Cenozoic.

    根据胶莱盆地区域地质特征,地球动力学背景及盆地中、新生代沉积特征分析,论述盆地的发育和演化阶段,并对胶莱盆地含油气前景进行探讨。

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  • Sedimentary environment and its evolution, distribution of sedimentary facies and sand bodies are discussed on the base of the data of log, drilling and c, o isotope.

    本文利用测井、钻井和C、O同位素等资料,研究了核二段各砂组沉积时期的沉积环境、相带分布、砂体展布以及沉积演化规律。

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  • Clastic sediments bears much information about the nature of source rocks and their tectonic evolution, which is significant for sedimentary basin analysis.

    碎屑沉积物记录着有关源岩性质和构造演化等诸多重要的信息,对于沉积盆地分析和理解区域构造演化都有重要的指示意义。

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  • The sedimentary history of Wuerxun Depression includes a few stages corresponding with structural evolution.

    乌尔逊凹陷沉积过程与构造演化对应,具有阶段性。

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  • This paper, in terms of sequence stratigraphy and sedimentary dynamics, deals with sequence filling succession and sedimentary dynamic evolution of Xichang Compound Basin.

    本文从层序地层学和沉积动力学角度,对西昌复合盆地进行了初步的研究。

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  • With the above models, the oil and gas evolution history in a sedimentary basin with complex lithology can be modeled.

    利用这一组模型。可以对既有碳酸盐岩又有碎屑岩的复杂岩性沉积盆地中的油气演化进行模拟。

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  • The constitution and evolution features of sedimentary facies and reservoir distribution rules are studied within the high frequency sequence.

    在高频层序内研究了沉积微相的构成与演化特征以及储层分布规律。

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