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相层序
相关语句
  facies sequence
    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 primary control factors of fluvial facies sequence forming are structure factor or palaeotopography, climate factor and sediment supply. It is possible that palaeotopography and climate factors influence fluvial facies sequence forming and development macrofeature more apparently.
    河流相层序形成的主控因素为构造因素(或古地形)、气候因素和沉积物补给,而古地形和气候因素对冲积—河流相层序形成与发育宏观特征的影响可能更为明显,在河流相层序地层分析中,基准面,而不是海(湖)平面是层序研究的主要参照面。
短句来源
    This article also summarizes facies mark, facies sequence, facies model and sandbody spreading character of lowstand delta.
    低位三角洲发育在主要物源区的前方 ,处在深湖相泥岩包围之中 ,相标志、相层序、相模式和砂体的展布特征有别于深水重力流沉积 ,是重要的油气储集体。 图 4参 18
短句来源
    Based on the log response of different sedimentary microfacies, the distribution character of the sedimentary facies in the plane is researched, and the facies sequence and pattern of this area are summed up.
    根据不同沉积微相的测井响应特征,研究了沉积相在平面上的分布特征,并总结出研究区的相层序和相模式。
短句来源
  facies sequence
    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 primary control factors of fluvial facies sequence forming are structure factor or palaeotopography, climate factor and sediment supply. It is possible that palaeotopography and climate factors influence fluvial facies sequence forming and development macrofeature more apparently.
    河流相层序形成的主控因素为构造因素(或古地形)、气候因素和沉积物补给,而古地形和气候因素对冲积—河流相层序形成与发育宏观特征的影响可能更为明显,在河流相层序地层分析中,基准面,而不是海(湖)平面是层序研究的主要参照面。
短句来源
    This article also summarizes facies mark, facies sequence, facies model and sandbody spreading character of lowstand delta.
    低位三角洲发育在主要物源区的前方 ,处在深湖相泥岩包围之中 ,相标志、相层序、相模式和砂体的展布特征有别于深水重力流沉积 ,是重要的油气储集体。 图 4参 18
短句来源
    Based on the log response of different sedimentary microfacies, the distribution character of the sedimentary facies in the plane is researched, and the facies sequence and pattern of this area are summed up.
    根据不同沉积微相的测井响应特征,研究了沉积相在平面上的分布特征,并总结出研究区的相层序和相模式。
短句来源
  facies sequence
    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 primary control factors of fluvial facies sequence forming are structure factor or palaeotopography, climate factor and sediment supply. It is possible that palaeotopography and climate factors influence fluvial facies sequence forming and development macrofeature more apparently.
    河流相层序形成的主控因素为构造因素(或古地形)、气候因素和沉积物补给,而古地形和气候因素对冲积—河流相层序形成与发育宏观特征的影响可能更为明显,在河流相层序地层分析中,基准面,而不是海(湖)平面是层序研究的主要参照面。
短句来源
    This article also summarizes facies mark, facies sequence, facies model and sandbody spreading character of lowstand delta.
    低位三角洲发育在主要物源区的前方 ,处在深湖相泥岩包围之中 ,相标志、相层序、相模式和砂体的展布特征有别于深水重力流沉积 ,是重要的油气储集体。 图 4参 18
短句来源
    Based on the log response of different sedimentary microfacies, the distribution character of the sedimentary facies in the plane is researched, and the facies sequence and pattern of this area are summed up.
    根据不同沉积微相的测井响应特征,研究了沉积相在平面上的分布特征,并总结出研究区的相层序和相模式。
短句来源
  “相层序”译为未确定词的双语例句
    CARBONIFEROUS SEQUENCE STRATIGRAPHY ON CLINOTHEM FACIES AT NANDAN AREA IN NORTHERN GUANGXI
    桂北南丹地区石炭纪斜坡相层序地层分析
短句来源
    Mechanism of allowable space change and its diagram in continental sequence, upper member
    泌阳断陷下第三系核三上段陆相层序可容空间变化机理及其图解
短句来源
    This paper studies the research method of sequence stratigraphy in fluvial facies by using high-resolution sequence stratigraphy relies on base-level cycle recognition.
    本论文以河流相沉积学研究为基础,运用以基准面旋回为参照面的高分辨率层序地层理论和研究方法分析了河流相层序地层单元的构成,探讨了河流相层序地层研究方法。
短句来源
    ②in deep-water sequences,the upper part of the transgressive systems tract and the lower part of highstand system tract have better quality of organic matter in relatively high abundance with an "S" shape organic factes sequence,and organic factes display obvious lateral variations;
    ②在深水型层序中,海进体系域上部和高位体系域下部有机质丰度较高、类型较好,有机相层序呈S性,但有机相的侧向变化明显;
短句来源
    Sedimentation in continental basins has been controlled by many factors and the main control factors in basins of different types are not the same. All these would lead to various sedimentation types,frequent facies changes,poor lateral continuity and large variation of sequence thickness.
    陆相层序地层与被动大陆边缘海相层序地层之间存在较大的差异。 陆相盆地沉积受多种因素控制 ,而且不同类型盆地的主要控制因素又各不相同 ,造就了陆相盆地沉积类型多、相变快、横向连续性差、纵向上层序厚度变化大 ,频繁的湖侵湖退使湖盆沉积垂向上韵律变化快 ;
短句来源
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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.
      


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。

Sequence stratigraphy provides an effective framework for basin-fill analysis and reservoir prediction,but little attention has been paid to its significance in source rock evaluation and prediction. Combined sequence stratigraphy and organic factes studies have conducted in Yinggehai and Qiongdongnan basins have yielded the following results:①in shallowwater sequences,each system tract has similar organic factes composition and no obvious lateral change in organic factes occurs; ②in deep-water sequences,the...

Sequence stratigraphy provides an effective framework for basin-fill analysis and reservoir prediction,but little attention has been paid to its significance in source rock evaluation and prediction. Combined sequence stratigraphy and organic factes studies have conducted in Yinggehai and Qiongdongnan basins have yielded the following results:①in shallowwater sequences,each system tract has similar organic factes composition and no obvious lateral change in organic factes occurs; ②in deep-water sequences,the upper part of the transgressive systems tract and the lower part of highstand system tract have better quality of organic matter in relatively high abundance with an "S" shape organic factes sequence,and organic factes display obvious lateral variations; ③the overall organic factes evolution trend of multiple sequences reflects the basin-fill process.This study confirms that the distribution model of Organic factes in a sequence framework is of great significance in predicting petroleum source rocks using seismic data and well logs.

层序地层学为沉积盆地的充填史分析和储层预测提供了有效的格架,但其在源岩评价和预测中的意义未能引起充分的重视。本文对莺歌海、琼东南盆地的各沉积层序进行了有机相分析,发现①浅水型沉积层序中各体系域的有机相构成基本相同,且有机相的侧向变化不明显;②在深水型层序中,海进体系域上部和高位体系域下部有机质丰度较高、类型较好,有机相层序呈S性,但有机相的侧向变化明显;③多层序有机相的总体演化趋势反映了盆地的充填演化过程。层序格架内有机相的分布模式对利用地震资料进行源岩预测具有重要意义。

Based on stratigraphy and sedimentology, the sequence stratigraphy of the clinothem facies in the Nandan area of northern Guangxi is analyzed. 11 sequences have been recognized. There are 2 sequences in Luzai Formation, 3 sequences in Baping Formation, 6 sequences in Nandan Formation. All of these sequences being formed in the deeper sea environment can be compared with those sequences being formed in the shallow sea platform environment in southern Guizhou. The signatures of the sequences in the clinothem...

Based on stratigraphy and sedimentology, the sequence stratigraphy of the clinothem facies in the Nandan area of northern Guangxi is analyzed. 11 sequences have been recognized. There are 2 sequences in Luzai Formation, 3 sequences in Baping Formation, 6 sequences in Nandan Formation. All of these sequences being formed in the deeper sea environment can be compared with those sequences being formed in the shallow sea platform environment in southern Guizhou. The signatures of the sequences in the clinothem facies and basin facies have been recognized. The sequences on clinothem make it possible to correlate the sequences on platform facies with the sequences on basin facies.

以层序地层学理论为指导,在地层学和沉积学研究的基础上,对桂北南丹地区石炭纪斜坡相地层进行了沉积层序分析,共识别出11个三级层序,其中鹿寨组2个,巴平组3个,南丹组6个,它们均可与黔南独山地区石炭纪台地相所识别出的11个三级层序对比.同时探讨了较深水斜坡乃至盆地沉积环境下层序的表现形式,斜坡相层序地层的建立是联系台地相和盆地相沉积层序的纽带.

 
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