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层序地层体制
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  sequence stratigraphic system
     In sequence stratigraphic system, vertical development of the reservoir is controlled by base level cycle changes, and spatial distribution is restricted by the palaeogeomorphology.
     在层序地层体制中,储层的纵向发育受基准面升降变化旋回的控制,而平面展布受古地貌的制约。
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  “层序地层体制”译为未确定词的双语例句
     THE REGULARITIES OF FORMATION AND DISTRIBUTION OF RESERVOIRS IN SYSTEMS OF CONTINENTAL SEQUENCE STRATIGRAPHY
     层序地层体制中的陆相储层发育规律
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  相似匹配句对
     THE REGULARITIES OF FORMATION AND DISTRIBUTION OF RESERVOIRS IN SYSTEMS OF CONTINENTAL SEQUENCE STRATIGRAPHY
     层序地层体制中的陆相储层发育规律
短句来源
     SEQUENCE STRATIGRAPHIC CHARACTERISTICS OF SICHUAN BASIN
     四川盆地层序地层特征
短句来源
     ON SEQUENTIAL STRATIGRAPHY PATTERN
     层序地层模式浅析
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     STRATUM
     地层
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Based on the principle of lithologic sequence,Dongying formation in Shenghai

根据基准面旋回变化控制层序地层形成和展布规律的基本原理,济阳坳陷胜海地区东营组由5个地层层序组成,并受两大沉积体系控制。在层序地层体制中,储层的发育在纵向上受基准面旋回变化的控制,形成于各层序单元的下部;在平面上受下切河谷、坡折带和地层上超尖灭等古地貌格局的制约。在目的层序中预测出4条浊积水道及其控制的6个有利的储油砂体,并得到了钻井的证实,获得成功

According to the analysis of seismic and well log sequence stratigraphy, four sequences are identified in Upper Paleozoic of north Ordos Basin, which are all separated by the regional erosion surfaces and channel washing surfaces. The characteristics of sequences reflect the process of evolution of the Ordos Basin which experimented the formation, development, waning and consumption of epicontinental basin. The offshore sandstone of Carboniferous and channel sandstone and alluvial fan of Permian are mainly...

According to the analysis of seismic and well log sequence stratigraphy, four sequences are identified in Upper Paleozoic of north Ordos Basin, which are all separated by the regional erosion surfaces and channel washing surfaces. The characteristics of sequences reflect the process of evolution of the Ordos Basin which experimented the formation, development, waning and consumption of epicontinental basin. The offshore sandstone of Carboniferous and channel sandstone and alluvial fan of Permian are mainly reservoir rocks. In sequence stratigraphic system, vertical development of the reservoir is controlled by base level cycle changes, and spatial distribution is restricted by the palaeogeomorphology. The distribution of advantageous reservoir is predicted on the basis of the comprehensive analysis of seismic profiles and well logs.

通过地震和测井层序地层分析,可在鄂尔多斯盆地北部上古生界识别出4个地震层序,层序界面均以区域性侵蚀面或河道冲刷面为边界。层序的发育特征反映了鄂尔多斯盆地在晚古生代经历了陆表海盆地的形成、发展、衰退和逐渐消亡的过程。储集层主要是石炭系的滨岸砂体、二叠系的河道砂体以及冲积扇砂体。在层序地层体制中,储层的纵向发育受基准面升降变化旋回的控制,而平面展布受古地貌的制约。通过地震与钻井的综合分析,具体预测出有利的储集砂体分布。

In order to increase the exploration level of hidden oil & gas pools in the area around Puwei sag, Dongpu depression, sequence stratigraphy theory and the Walther's law are taken as a guide to research Sha 3 member. On the basis of the analyses of cores, logs and seismic data, combined with the analyses of basin structure and stratigraphy, 5 depositional systems are recognized in Sha 3 member, i. e. lake turbidite fan system, coast & shallow lake system with sand dam and tempestite, low stand salt lake system,...

In order to increase the exploration level of hidden oil & gas pools in the area around Puwei sag, Dongpu depression, sequence stratigraphy theory and the Walther's law are taken as a guide to research Sha 3 member. On the basis of the analyses of cores, logs and seismic data, combined with the analyses of basin structure and stratigraphy, 5 depositional systems are recognized in Sha 3 member, i. e. lake turbidite fan system, coast & shallow lake system with sand dam and tempestite, low stand salt lake system, delta system and deep & hemi deep lake system. The characteristics of lithoface assemblages of each system are studied one by one. The distribution patterns of the depositional systems in space are analysed in each main reservoir body member, while the sedimentary models and reservoir distribution regulations of the Sha 3 member are also discussed. It is pointed out that the junctions of the under water channels and the slope break belt in the east and north of Puwei sag are the places where the main reservoir bodies develop very well, and where lake turbidite fan system and delta system develop.

为了提高东濮凹陷濮卫环洼带隐蔽油气藏的勘探精度 ,以层序地层学理论和瓦尔特相律为指导 ,通过钻井岩芯、测井和地震的三元分析法 ,综合构造—地层分析 ,在东濮凹陷濮卫环洼带沙三段共识别出湖底扇、滨浅湖砂坝—风暴、低位盐湖、三角洲、深湖—半深湖等五种沉积体系 ,分析了主要储层发育期沉积体系的时空展布特征 ,探讨了层序地层体制下沙三段的沉积体系发育模式及储层发育规律 ,指出环洼带东部及北部水下河道与坡折带的交汇处是储层的主要发育地带 ,其沉积体系主要为湖底扇、三角洲沉积体系

 
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