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相层序
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  facies sequence
    STUDY ON ALLUVIAL-FLUVIAL FACIES SEQUENCE STRATIGRAPHY
    冲积-河流相层序地层学研究
短句来源
    Discussion on the stratigraphic model in alluvial-fluvial facies sequence and its application in Jiyang depression.
    冲积—河流相层序地层模式探讨及其在济阳坳陷的应用
短句来源
    Study on Alluvial-Fluvial Facies Sequence Stratigraphy and Favorable Reseivoir Zones Prediction for Neogene, Inshore Area, Jiyang Depression
    济阳坳陷滩海地区新近系冲积-河流相层序地层研究与有利成藏区带预测
短句来源
    The Distribution of Sedimentary Organic Facies in the Continental Facies Sequence Stratigraphic Framework: an example from Middle Jurassic coal bearing series in the Taibei sag of the Turpan Hami basin and Southern Junggar basin
    沉积有机相在陆相层序地层格架中的分布特征——以吐哈盆地台北凹陷及准噶尔盆地南缘中侏罗世煤系为例
短句来源
    Fluvial Facies Sequence Stratigraphy Discuss
    河流相层序地层学研究
短句来源
更多       
  facies sequence
    STUDY ON ALLUVIAL-FLUVIAL FACIES SEQUENCE STRATIGRAPHY
    冲积-河流相层序地层学研究
短句来源
    Discussion on the stratigraphic model in alluvial-fluvial facies sequence and its application in Jiyang depression.
    冲积—河流相层序地层模式探讨及其在济阳坳陷的应用
短句来源
    Study on Alluvial-Fluvial Facies Sequence Stratigraphy and Favorable Reseivoir Zones Prediction for Neogene, Inshore Area, Jiyang Depression
    济阳坳陷滩海地区新近系冲积-河流相层序地层研究与有利成藏区带预测
短句来源
    The Distribution of Sedimentary Organic Facies in the Continental Facies Sequence Stratigraphic Framework: an example from Middle Jurassic coal bearing series in the Taibei sag of the Turpan Hami basin and Southern Junggar basin
    沉积有机相在陆相层序地层格架中的分布特征——以吐哈盆地台北凹陷及准噶尔盆地南缘中侏罗世煤系为例
短句来源
    Fluvial Facies Sequence Stratigraphy Discuss
    河流相层序地层学研究
短句来源
更多       
  facies sequence
    STUDY ON ALLUVIAL-FLUVIAL FACIES SEQUENCE STRATIGRAPHY
    冲积-河流相层序地层学研究
短句来源
    Discussion on the stratigraphic model in alluvial-fluvial facies sequence and its application in Jiyang depression.
    冲积—河流相层序地层模式探讨及其在济阳坳陷的应用
短句来源
    Study on Alluvial-Fluvial Facies Sequence Stratigraphy and Favorable Reseivoir Zones Prediction for Neogene, Inshore Area, Jiyang Depression
    济阳坳陷滩海地区新近系冲积-河流相层序地层研究与有利成藏区带预测
短句来源
    The Distribution of Sedimentary Organic Facies in the Continental Facies Sequence Stratigraphic Framework: an example from Middle Jurassic coal bearing series in the Taibei sag of the Turpan Hami basin and Southern Junggar basin
    沉积有机相在陆相层序地层格架中的分布特征——以吐哈盆地台北凹陷及准噶尔盆地南缘中侏罗世煤系为例
短句来源
    Fluvial Facies Sequence Stratigraphy Discuss
    河流相层序地层学研究
短句来源
更多       
  “相层序”译为未确定词的双语例句
    LOESS AND OTHER SUBAERAL SEQUENCES IN THE MIDDLE DANUBIAN BASIN
    多瑙河中游盆地黄土和其它陆相层序
短句来源
    THE SEQUENCE STRATIGRAPHY OF TERRESTRIAL FACIES OF THE TUNXI BASIN IN SOUTH ANHUI
    皖南屯溪盆地陆相层序地层学特征
短句来源
    STUDY ON CRETACEOUS STRATIGRAPHIC SEQUENCE OF CONTINENTAL BASIN IN JIANGSU
    江苏白垩纪陆相层序地层研究
短句来源
    Understandings of the continental sequence stratigraphy——An example from 1∶50000 regional survey of Minhe basin,Gansu Province
    对陆相层序地层的一些认识——以甘肃民和盆地1∶5万区域地质调查为例
短句来源
    Continental Sequence Stratigraphy Study of Gaoyou Sag in Subei Basin.
    苏北盆地高邮凹陷陆相层序地层研究
短句来源
更多       
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  facies sequence
Contrary to expectations, the re-establishment of a complete but compressed facies sequence incorporating mud flats and salt marshes has not materialized.
      
This facies sequence, deposited on a relatively uniform and gentle basin slope, indicates that the area was a homoclinal ramp which has modern counterparts in the Persian Gulf and Shark Bay, Australia.
      
Transgressive facies sequence of a high energy, wave-tide-storm-influenced shoreface: A case study of the east Frisian Barrier I
      
Depositional relief on the buildups was as much as 70 feet based on the vertical facies sequence.
      
  facies sequence
Contrary to expectations, the re-establishment of a complete but compressed facies sequence incorporating mud flats and salt marshes has not materialized.
      
This facies sequence, deposited on a relatively uniform and gentle basin slope, indicates that the area was a homoclinal ramp which has modern counterparts in the Persian Gulf and Shark Bay, Australia.
      
Transgressive facies sequence of a high energy, wave-tide-storm-influenced shoreface: A case study of the east Frisian Barrier I
      
Depositional relief on the buildups was as much as 70 feet based on the vertical facies sequence.
      
  facies sequence
Contrary to expectations, the re-establishment of a complete but compressed facies sequence incorporating mud flats and salt marshes has not materialized.
      
This facies sequence, deposited on a relatively uniform and gentle basin slope, indicates that the area was a homoclinal ramp which has modern counterparts in the Persian Gulf and Shark Bay, Australia.
      
Transgressive facies sequence of a high energy, wave-tide-storm-influenced shoreface: A case study of the east Frisian Barrier I
      
Depositional relief on the buildups was as much as 70 feet based on the vertical facies sequence.
      


Current- meter data collected over the past 20 years has revealed the existence of currents flowing alternatively up and down most submarine canyons and other submarine valleys. These currents are attributed to internal weaves that are subsurface waves between layers of different density or within layers where vertical density gradients are present. An important kind of internal wave is that which has a period equal to the semidiurnal or diurnal tide and referred to as an internal tied. Velocities of bidirectional...

Current- meter data collected over the past 20 years has revealed the existence of currents flowing alternatively up and down most submarine canyons and other submarine valleys. These currents are attributed to internal weaves that are subsurface waves between layers of different density or within layers where vertical density gradients are present. An important kind of internal wave is that which has a period equal to the semidiurnal or diurnal tide and referred to as an internal tied. Velocities of bidirectional deep-water currents range from 20-50 cm / sec. Such currents can move sediment up to fine sand and form a lot of ripples at depths of several thousand meters. Nevertheless, internal-tied deposits have not been recognized in the ancient rock record.

本文论述了在世界范围内首次鉴别出的新的沉积类型——内潮汐沉积,发现于美国弗吉尼亚州芬卡苏地区奥陶纪深水海底水道充填沉积中。已识别出两种相:①双向交错纹理极细砂岩相,以发育分别向古水道上方和下方倾斜的双向交错纹理为特征,被归因于内潮汐作用沉积的产物。②单向交错层和交错纹理中至细砂岩相,发育向古水道上方倾斜的低角度板状交错层和交错纹理,被解释为叠加有内波的内潮汐沉积物。据沉积相层序分析,内潮汐沉积形成于海平面上升、粗屑重力流受到抑制的时期。

Aiming at the characteristics of the Mesozoic and Cenozoic terrestrial basins in China, the paper discusses the control of the relative change of lake level, supply of sediments and climate on the lake sequence strata in light of the influence of the sedimentary basinstructure and margin setting on the marine sequence strata. It points out that the methods of the marine sequence stratigraphy can not be used indiscriminately in the analysis of the inland basins owing to the essential differences between the marine...

Aiming at the characteristics of the Mesozoic and Cenozoic terrestrial basins in China, the paper discusses the control of the relative change of lake level, supply of sediments and climate on the lake sequence strata in light of the influence of the sedimentary basinstructure and margin setting on the marine sequence strata. It points out that the methods of the marine sequence stratigraphy can not be used indiscriminately in the analysis of the inland basins owing to the essential differences between the marine and inland settings.

针对中国中、新生代陆相湖盆的特征,从沉积盆地的构造和边缘背景对海相层序地层的影响出发,讨论了湖水面相对变化、沉积物供给、气候等对湖相层序地层的控制作用,明确指出两种背景条件具有本质差异,海相层序地层学方法不能简单套用于内陆盆地分析。

An organic factes is defined as a mappable stratigraphic unit containing organic matter (OM)of a particular genetic type in cartaain abundance. A new organic factes classification, which is based on indicative genetic kerogen (OM) type, is proposed. The improved definition and classification makes organic factes capable of reflecting the origin. diagenetic alternation of organic matter comprehensively, and, the organic facies thus defined and classified, which must be identified on the basis of synthetical parameters...

An organic factes is defined as a mappable stratigraphic unit containing organic matter (OM)of a particular genetic type in cartaain abundance. A new organic factes classification, which is based on indicative genetic kerogen (OM) type, is proposed. The improved definition and classification makes organic factes capable of reflecting the origin. diagenetic alternation of organic matter comprehensively, and, the organic facies thus defined and classified, which must be identified on the basis of synthetical parameters other than by atomic H/C ratios and/or Rock-Eval Hydrogen index values merely. Several new concepts concerning organic factes such as Vertical Organic Facies Sequence (VOFS), Organic Facies Association(OFA) and Organic Basin - fill Sequence (OBFS) are advanced, and their significance in basin analysis is discussed in detail.Several cases are presented in this peper which confirm that organic facies, especially VOFS, OFA and OBFS analysis Can not only become a very use full tool for prediction and three-dimensional mapping of petroleum source rocks. but also make up for some Shortcomings of sedimentological studies that put the stress on coarse rocks, and therefore may play a distinctive role in identifying and accurately locating unconformities or sequence/ systems tract boundaries as well as in reconstructing the tectonic subsidence and sedimentary fill histories of sedimentary basins.

有机相是具有一定丰度和特定成因类型的有机质的地层单元,决定有机相类型的最重要参数是干酪根的成因类型。为了反映沉积盆地中有机相的时空分布,我们提出了有机相组合和盆地有机充填序列等新概念。有机相及有机相层序、有机充填序列和有机相组合不仅是预测和在三维空间确定生油岩的分布、预测主力生油岩的排烃期和排出产物的组成的有效工具,而且可以弥补以骨架砂岩体为主要研究对象的沉积学分析的不足,在确定层序界线或不整合面的位且、研究盆地的构造沉降和沉积充填史等方面发挥重要作用。

 
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