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层序成因     
相关语句
  sequence genesis
     Moreover,the analysis of sequence genesis has also revealed that lake-level changes are not synchronized with or correlative with sea-level fluctuations.
     层序成因分析同时还揭示陆相断陷盆地的湖平面变化与海平面变化不同步及没有可比性。
短句来源
     The concept of depositional accommodation has been applied to sequence genesis analysis and sequence division for continental rift basins with examples from Paleogene,Bohaiwan basin.
     以渤海湾盆地下第三系为例,将可容纳空间概念应用于陆相断陷盆地层序成因分析和层序划分。
短句来源
     By the cognition that sequence development of rifting basin is mainly controlled by synsedimentary fault and fundamental subsidence,relationship between sequence genesis and basin structure has been set up. The sequence framework and filling proccess are obviously distinct within different genetic basins.
     通过对裂谷盆地层序发育明显受同沉积断裂及基底沉降控制的分析 ,建立了层序成因与盆地构造活动的关系模型。
短句来源
     According to the sequence genesis dynamics, the consistency of cycle properties and the difference of boundary properties respectively indicate that the sedimentary environments control the sediment types in the same sequence stratigraphic framework and the migration of tectonic depoccnters and sedimentary centers in the Bohai Bay Basin controls the sequence boundary properties.
     从层序成因动力学角度来解释,这种旋回性质的相似性和界面性质的差异性分别表明了:同一层序地层格架中沉积环境对沉积物类型起决定性的影响作用,以及渤海湾盆地构造沉降、沉积中心的迁移对层序界面性质具有主要的控制作用。
短句来源
  sequence genetic
     Parameter Type of Sequence Genetic Dynamics and Its Significance
     层序成因动力学参数类型及意义
短句来源
     In terms of sequence-basin-tectonics, the tectonics controls the sequence genetic dynamics.
     以层序—盆地—构造为主线 ,对层序成因动力学中的构造控制进行了研究。
短句来源
     STUDY ON TECTONIC CONTROLS IN SEQUENCE GENETIC DYNAMICS
     层序成因动力学中的构造因素研究
短句来源
     Based on the research on relationship between oil and gas trap distribution and sequence framework of Upper Paleozoic in Southwest China,the authors suggest that oil-gas trap type,characteristics of sequence genetic framework and internal architecture of distinct genetic basins are quite different.
     西南地区上古生界层序格架与油气圈闭关系研究表明,不同成因类型沉积盆地的层序成因格架和内部构型各异; 不同层序的油气圈闭特征及分布存在明显差异.
短句来源
     SEQUENCE GENETIC FRAMEWORK AND RESERVOIR DISTRIBUTION OF LOWER PERMIAN IN
     右江裂谷盆地下二叠统层序成因格架与储层分布
短句来源
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  cause of sequence formation
     Based on discussing about isotape age, biostratigraphic correlation, cause of sequence formation, sequence stratigraphic correlation and sequence boundary, sequence stratigraphic framework can not be regarded as isochronous, so it can not be regarded as the standard of global correlation, it reflects the spreading rule of sedimental action and sedimental strata in three-dimensional space.
     通过对同位素测年、生物地层对比、层序成因、层序地层对比及层序界面性质五个方面的讨论 ,指出层序地层格架不是一个等时地层格架 ,不能作为全球对比的标准 ,它所体现的主要是沉积作用和沉积地层在三维空间的展布规律。
短句来源
  “层序成因”译为未确定词的双语例句
     3)Tectonic natures control the basin characteristics and then the genetic framework and boundary type of sequence;
     3)构造属性控制盆地性质 ,进而控制层序成因格架和界面成因类型 ;
短句来源
     GENESIS OF STRATIGRAPHIC SEQUENCE IN CONTINENTAL RIFT BASINS
     陆相断陷盆地层序成因初探
短句来源
     The origin of the third-ordercycle sequences in foreland basins are obviously controlled by regional tectonism adjacent tothe orogenic belt,sedimentation within the basins and the relative sea-level fluctuation.
     前陆盆地三级层序成因并非受全球统一的海平面变化控制,而是与盆缘造山带区域构造运动、盆内沉积作用和相对海平面变化的联合作用有关,代表了前陆盆地一个成盆期的不同发育阶段。
短句来源
     Sequence stratigraphic study of petroliferous provinces,genesis of nonmarine sequences,and high-resolution sequence stratigraphic study should be enhanced in hydrocarbon exploration practices of China in the 21st century,in order to serve for discovering new petroliferous sags and strata and finding subtle traps and new reserves in “matured” exploration regions
     在 2 1世纪我国油气勘探实践中 ,应加强含油气大区层序地层学、陆相层序成因与高分辨率层序地层学研究 ,为寻找新的含油气凹陷与含油气层系、寻找隐蔽圈闭与老区挖潜服务。
短句来源
     A preliminary genesis analysis about a stratigraphic sequence showed that the development of sequence in confinental rift basins is just controlled by episode tectonic subsidence,and not sea/lake-level changes.
     层序成因初步分析表明,陆相断陷盆地的层序形成机制不是海(湖)平面变化,而是幕式构造沉降作用。
短句来源
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  sequence genetic
Sequence genetic analysis points to the diversification of different HCV genotypes 200 to 400 years ago.
      
  sequence origin
Extensive work on n-tuplet occurrence in genomic sequences has revealed the correlation of their usage with sequence origin.
      
Analyses of all the related sequences in a large, formatted protein sequence space suggest that many, if not all, of the 27 omnipresent elements have a common sequence origin.
      


Sequence stratigraphy of foreland basin is a special application of the theory of sequence stratigraphy to the tectonically active foreland basins.The origin of the third-ordercycle sequences in foreland basins are obviously controlled by regional tectonism adjacent tothe orogenic belt,sedimentation within the basins and the relative sea-level fluctuation.Thesequence boundary is an interplay of relative sea-level drop and local tectonic uplift.n theasymmetric subsidence filling stage of foreland basin evolution,there...

Sequence stratigraphy of foreland basin is a special application of the theory of sequence stratigraphy to the tectonically active foreland basins.The origin of the third-ordercycle sequences in foreland basins are obviously controlled by regional tectonism adjacent tothe orogenic belt,sedimentation within the basins and the relative sea-level fluctuation.Thesequence boundary is an interplay of relative sea-level drop and local tectonic uplift.n theasymmetric subsidence filling stage of foreland basin evolution,there are two types of sequences.Lowstand turbidite fan sequence is on the proximal side to the orogenic belt.Awayfrom the orogenic belt,erosional sequence boundaries and transgressive surfaces are merged,with no record of lowstand system tracts,or with a few of shelf margin system tracts underthe transgressive surface.Each sequence is composed of transgressive system tract,condensedsection,early highstand system tract and late highstand system tract.

前陆盆地层序地层学是将层序地层学理论应用于构造活动的前陆盆地分析的一个特例。前陆盆地三级层序成因并非受全球统一的海平面变化控制,而是与盆缘造山带区域构造运动、盆内沉积作用和相对海平面变化的联合作用有关,代表了前陆盆地一个成盆期的不同发育阶段。层序界面是相对海平面下降和区域构造隆升的联合作用面。在盆地演化的不对称沉降充填阶段,邻造山带区为低水位浊积扇沉积层序;远离造山带区,低水位体系域不发育,或有少量相当于低水位沉积的陆架边缘体系域,且低水位剥蚀面与海侵面往往合二为一。在层序组成上,自下而上为海侵体系域、凝缩层、早期高水位体系域和晚期高水位体系域。

A preliminary genesis analysis about a stratigraphic sequence showed that the development of sequence in confinental rift basins is just controlled by episode tectonic subsidence,and not sea/lake-level changes. The second order tectonic cycles control the development of sequences while the third and the forth order tectonic cycles are the main control factors of the development of parasequence sets and most parasequences respectively. The ratio between the new space added by tectonic subsidence and the volume...

A preliminary genesis analysis about a stratigraphic sequence showed that the development of sequence in confinental rift basins is just controlled by episode tectonic subsidence,and not sea/lake-level changes. The second order tectonic cycles control the development of sequences while the third and the forth order tectonic cycles are the main control factors of the development of parasequence sets and most parasequences respectively. The ratio between the new space added by tectonic subsidence and the volume of supplied or filled corresponding sediment determines the type and the characteristics of parasequences , parasequence sets and depositional systems tracts. The development of the main sequence surfaces,such as the unconformity and hiatus ,for dividing different order sequences in continental rift basins,is related to tectonic events. Moreover,the analysis of sequence genesis has also revealed that lake-level changes are not synchronized with or correlative with sea-level fluctuations.

层序成因初步分析表明,陆相断陷盆地的层序形成机制不是海(湖)平面变化,而是幕式构造沉降作用。二级构造旋回控制层序的发育,三级、四级旋回分别是准层序组;大多数准层序形成的主导控制因素、构造沉降新增沉积空间与同期供给或充填盆地的沉积物体积之间的对比关系,决定了准层序、准层序组和体系域的类型和特征。作为划分陆相断陷盆地各级层序的主要界面,如不整合面、沉积间断面等,其形成与构造作用有关。层序成因分析同时还揭示陆相断陷盆地的湖平面变化与海平面变化不同步及没有可比性。

The Permian sedimentary basins in the Hunan Hubei Jiangxi region are developed on the ground of the unified South China continental block.According to crustal activity,sediment filling sequences,sedimentary facies belts and their spatial arrangement,the sedimentary basins in this region may be divided into Yangtze cratonic basin,passive marginal basin on the northern margin of the Yangtze craton,Hunan Jiangxi intraplate extensional basin and Cathaysian pericratonic basin.The differences of the controlling...

The Permian sedimentary basins in the Hunan Hubei Jiangxi region are developed on the ground of the unified South China continental block.According to crustal activity,sediment filling sequences,sedimentary facies belts and their spatial arrangement,the sedimentary basins in this region may be divided into Yangtze cratonic basin,passive marginal basin on the northern margin of the Yangtze craton,Hunan Jiangxi intraplate extensional basin and Cathaysian pericratonic basin.The differences of the controlling factors and associated effects upon the sequence development are responsible for the differences of sequence development.The present paper deals in details with the genesis and characteristics of the depositional sequences and depositional systems tracts in various sedimentary basins in the study area,and the regional correlations are also made in this paper.

湘鄂赣二叠纪沉积盆地是在统一的陆板块——华南陆块基础上发展而来的。根据晚古生代以来的地壳活动情况、沉积物充填序列、沉积相带及空间配置,该区可以划分为四种沉积盆地,即扬子克拉通盆地、扬子克拉通北缘被动大陆边缘盆地、湘赣板内拉张盆地和华夏克拉通边缘盆地。由于不同沉积盆地中层序发展的主控因素及其相关效应的差异,从而决定了层序发育特点的差异。本文详细划分了各种沉积盆地的沉积层序和沉积体系域,并进行了区域对比。在此基础上,探讨了层序的成因

 
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