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层序构成
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  sequence architecture
     Sequence Architecture and Favorable Reservoir Prediction of Sanya Formation in the Central and Eastern Qiongdongnan Basin
     琼东南盆地中东部三亚组层序构成及有利区带预测
短句来源
     Eocene Sequence Architecture and Controls of Sha 4 Member, in Southwest Dongying Depression, Bohai Bay Basin
     博兴洼陷沙四段层序构成样式及其主控因素
短句来源
     The sequence architecture and the distribution of depositional systems tracts were mainly controlled by a variety of tectonic activities during the formation and evolution of the basins.
     层序构成和沉积体系域的发育分布受到盆地形成演化过程中各种构造作用的控制。
短句来源
  sequence consists
     The deposition of system tract or the distribution of lithofacies was controlled by both the water level (high or low)and the tectonic subsidence,so that each sequence consists of transgressive regressive sedimentary cycle.
     体系域的沉积或岩相的分布明显受湖水升降及构造沉降的双重作用控制,每一层序构成了水进到水退的沉积旋回。
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  “层序构成”译为未确定词的双语例句
     The sequence stratigraphy,sedimentology and petroleum geology were used to study the architectural model of sequence stratigraphy controlling the distribution of litho-trap in deep-water lake of Songliao depressive basin.
     运用层序地层学、沉积学及石油地质学理论 ,研究了松辽盆地深水坳陷湖盆期 (青山口组到嫩江组沉积时期 )的层序构成模式对岩性圈闭分布的控制 ,结果表明 ,青山口组到嫩江组沉积时期 ,松辽盆地为深水坳陷湖盆。
短句来源
     The sequence stratigraphic units in Changtu Sag include three supersequences(SSⅠ,SSⅡ,SSⅢ),and the supersequence SSⅡ can be divided into two sequences(SⅡ 1 and SⅡ 2). Based on the tectonic movement and basin_filling sequence in Changtu Sag,the sequences are farther divided into lowstand system tract,expansion and contraction system tract of lake_basin.
     据构造活动及沉积层序充填特征分析 ,昌图凹陷地层层序可以划分为裂陷 (SSⅠ )、断陷 (SSⅡ )和坳陷 (SSⅢ )3个超层序 ,其中SSⅡ由SⅡ1、SⅡ2 两个层序构成
短句来源
     1. According to comprehensive analysis of regional plates motion and deep structure of the basin, basin filling characters, paleotectonic surfaces, Shiwufault depression has experienced three evolutionary phases.
     本课题以十屋断陷深部断陷层系为研究对象,对盆地构造—充填演化进行整体性分析,并重点研究典型的同沉积构造、反转构造样式以及层序构成样式,建立盆地构造格架和深层等时地层格架。
短句来源
     This sedimentary sequence is composed of 9 Rank III and 3 Rank II sub-sequences, reflecting short term (cycle III and cycle II) sea level changes.
     这个沉积序列由9个Ⅲ级层序和3个Ⅱ级层序构成,反映了短周期(Ⅲ和Ⅱ级周期)的海平面变化。
短句来源
     EPSODIC TECTONIC CYCLES AND INTERNAL ARCHITECTURES OF SEQUENCES IN CONTINENTAL BASIN
     陆相盆地幕式构造旋回与层序构成
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  相似匹配句对
     They are also involved in two supersequences.
     三级层序构成两个超层序
短句来源
     Architecture Model of Sequence Stratigraphy in Fluvial Facies
     河流相层序地层构成模式探讨
短句来源
     hardware constitution;
     硬件构成;
短句来源
     The Composition of the Plot
     情节的构成
短句来源
     (3) sequence stratigraphy;
     层序地层学;
短句来源
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  sequence architecture
Stratal patterns in the southwestern margin of the Ulleung Basin off southeast Korea: sequence architecture controlled by back-a
      
Figure 4.3 Schematic representation of the Montanyana Group sequence architecture in the Tremp thrust-sheet top basin.
      
However, in stratigraphic analysis their influence on sequence architecture is commonly neglected.
      
On the basis of sequence architecture, the remaining 871 loci represented putative ARMD events in the human lineage.
      
Seal potential and sequence architecture in the Vulcan Sub-Basin, NW Shelf, Australia.
      
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  sequence consists
The deduced amino acid sequence consists of 509 amino acid residues and shares 74~81% identity with those of ALDH7Bs from other plants.
      
Its complete genomic sequence consists of more than 11 000 bp encoding more than 3 700 amino acids.
      
The corresponding BACE2 sequence consists of a weakly positive domain directly upstream of a strongly positive domain, near a functionally active domain.
      
The derived amino acid sequence consists of 1 590 residues, and it is homologous to all fungal AROM proteins studied so far.
      
The OsGAPDH sequence consists of 1,772?bp with the longest open reading frame encoding 499 amino acids with a calculated relative mass of 54.2?kDa.
      
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The Luanhe River, 1,200 kilometers long, flows through the Yanshan mountains into the Bohai Bay, with an annual water discharge of 4.55 billion cubic meters and sediment discharge of 19 million tons. An alluvial fan-delta, covering an area of 2,500 square kilometers, is formed at the foot of Yanshan mountains along the shore of Bohai Sea. The northern part of the complex consists of two upwairdfining post-glacial sedimentary sequences,in which no marine faunas are found; while in the southern part, the post-glacial...

The Luanhe River, 1,200 kilometers long, flows through the Yanshan mountains into the Bohai Bay, with an annual water discharge of 4.55 billion cubic meters and sediment discharge of 19 million tons. An alluvial fan-delta, covering an area of 2,500 square kilometers, is formed at the foot of Yanshan mountains along the shore of Bohai Sea. The northern part of the complex consists of two upwairdfining post-glacial sedimentary sequences,in which no marine faunas are found; while in the southern part, the post-glacial formations are made up of an upward-fining sequence in the lowerpart and an upward-coarsing sequence in the upper part, both containing marine faunas. The lower part of the post-glacial sequence was deposited in the courseof transgression. With the rise of sea level and the datum plane in post-glacial time, sea water advanced into the land along the river valley. At the same time, accumulation of retrogressive deposits took, place in the lower reaches that filled in the river valley and formed the lower part of the sequence. The distance covered by retrogressive accumulations far excee dedthat of sea water. Marine faunas can only be found in the sequence within the reach of sea water, beyond which are continental beds without such fossils. Therefore, the transgressive sequences in the valley, with or withoutmarine faunas, are formed in a unified sedimentary process, so that the fluvial deposits in the north and the deltaic deposits in the south that constitute the upper part of the postglacial sequence are genetically related.

滦河经燕山山脉流入渤海,全长1200公里,年迳流量45.5亿米~3,年输沙量1900万吨。滦河于滦县出山口,在燕山山麓渤海之滨形成了面积约2500平方公里的冲积扇一三角洲。滦河冲积扇—三角洲的北部,冰后期沉积层由两个下粗上细的沉积层序构成,其中未发现海相生物,南部则由下段的下粗上细和上段的下细上粗层序构成,且含海相生物微体化石。冰后期沉积层的下部是在海进过程中形成的。冰后期海面上升,基面抬高,海水沿河进侵,同时河流下游出现溯源堆积。溯源堆积使河流充填,产生冰后期沉积层下部沉积层序。溯源堆积的距离远远超过海水溯河而上所能达到的距离。在海水影响可以到达的地方,海进河床充填层序含海相微体生物,而溯源堆积可以到达,而海水影响所不及的地方,海进河流充填层序不含海相生物,为陆相层。因此,海进河床充填层序,不论其含海相生物与否,都是由统一的沉积过程形成的。冰后期沉积层的上段,北部为河流层序,南部为三角洲层序,二者是在海退过程中沉积的,其成因联系是显而易见的。三角洲系海退沉积,但其形成是以海进作为前导,并由海进转化为海退。由此,滦河冲积扇—三角洲是成因上互相联系的。

The HongliuHe Ophiolite Suite which has just recently been discovered is situated on the boundary between Xinjiang and Ganshu Province geographically. The Ophiolite is composed of the seguence from lherzolite, harzburgite, cumulate complex, and diabase to lower and upper pillows lavas accompanied by jasper. It has been proved by the evidences of geology and fossils that it was developed on the northeastern margin of TaliMu palaeo-continent in mid-upper Silurian Epoch(S_(2-3)).Therefore, possesses many characteristics...

The HongliuHe Ophiolite Suite which has just recently been discovered is situated on the boundary between Xinjiang and Ganshu Province geographically. The Ophiolite is composed of the seguence from lherzolite, harzburgite, cumulate complex, and diabase to lower and upper pillows lavas accompanied by jasper. It has been proved by the evidences of geology and fossils that it was developed on the northeastern margin of TaliMu palaeo-continent in mid-upper Silurian Epoch(S_(2-3)).Therefore, possesses many characteristics differenr from those occurring in Mid-Ocean Ridge and indicafive of a tectonic setting of continent margin. For example,One can see the xenoliths in-cluding those rocks of continent basement and their thermal metamorphism as well as the action of water attributalle to the tear of the continental crusl. The petrochemistry and geochemistry also suggest that magma from the upper mantle passed through the continental crust and underwent violent contamination. In addition,the ophiolite demonstrates the relation between ZhongTianShan tectonic zone and TaliMu palaeo-Continent, that is, before mid-upper Siurian had taken shape they may haue leen an entirety,but,after that,TaliMu palaeo-continent remained unchanged while ZhongTianshan evolved to be an island arc in the Devonian-carboniferrous period.

近年发观的红柳河蛇绿岩套,在地理上位于新疆和甘肃两省区的边界上。该岩套由一个从二辉榄橄岩、方辉橄榄岩、堆积杂岩和辉绿岩到伴有碧玉硅质岩的上、下枕状熔岩层序构成,根据地质证据和化石证据证明,这个蛇绿岩发育在古塔里木大陆东北缘,时代为中—上志留世,因此它具有许多不同于产出在大洋中脊的蛇绿岩特征监暗示出大陆边缘这样一种构造背景。例如,人们可以看到一些包括大陆基底岩石在内的捕虏体和它们的热变质作用以及可归因于大陆壳撕裂的水的作用。岩石学和地球化学还表明来自上地幔的岩浆穿过陆壳监经历了强烈的混染作用。此外,它还说明中天山构造带和塔里木古陆之间的关系是:蛇绿岩形成的中上志留世以前,它们两者是一个整体,那之后,塔里木古陆维持原状,而中天山则在泥盆—石炭纪演化成—岛弧。

The HongliuHe Ophiolite Suite which has just recently been discovered is situated on the boundary between Xinjiang and Ganshu Province geographical- ly.The Ophiolite is composed of the seguence from lherzolite,harzburgite, cumulate complex,and diabase to lower and upper pillows lavas accompanied by jasper.It has been proved by the evidences of geology and fossils that it was developed on the northeastern margin of TaliMu palace-continent in mid- upper Silurian Epoch(S_(2-3)).Therefore,possesses many characteristics...

The HongliuHe Ophiolite Suite which has just recently been discovered is situated on the boundary between Xinjiang and Ganshu Province geographical- ly.The Ophiolite is composed of the seguence from lherzolite,harzburgite, cumulate complex,and diabase to lower and upper pillows lavas accompanied by jasper.It has been proved by the evidences of geology and fossils that it was developed on the northeastern margin of TaliMu palace-continent in mid- upper Silurian Epoch(S_(2-3)).Therefore,possesses many characteristics differ- enr from those occurring in Mid-Ocean Ridge and indicafive of a tectonic setting of continent margin.For example,One can see the xenoliths in-cluding those rocks of continent basement and their thermal metamorphism as well as the action of wator attributalle to the tear of the continental crusl.The petr- ochemistry and geochemistry also suggest that magma from the upper mantle passed through the continental crust and underwenk violent contamination.In addition,the ophiolite demonstrates the relation between ZhongTianShan tectonic zone and TaliMu palaeo-Continont,that is before mid-upper Siurian had ta- ken shape they may haue leen an entirety,but,after that,Tali Mu palace-continent remained unchanged while ZhongTianshan evolved to be an island are in the Devonian-carboniferrous period.

近年发观的红柳河蛇绿岩套,在地理上位于新疆和甘肃两省区的边界上。该岩套由一个从二辉榄橄岩、方辉橄榄岩、堆积杂岩和辉绿岩到伴有碧玉硅质岩的上、下枕状熔岩层序构成,根据地质证据和化石证据证明,这个蛇绿岩发育在古塔里木大陆东北缘,时代为中—上志留世,因此它具有许多不同于产出在大洋中脊的蛇绿岩特征并暗示出大陆边缘这样一种构造背景。例如,人们可以看到一些包括大陆基底岩石在内的捕虏体和它们的热变质作用以及可归因于大陆壳撕裂的水的作用。岩石学和地球化学还表明来自上地幔的岩浆穿过陆壳并经历了强烈的混染作用。此外,它还说明中天山构造带和塔里木古陆之间的关系是:蛇绿岩形成的中上志留世以前,它们两者是一个整体,那之后,塔里木古陆维持原状,而中天山则在泥盆—石炭纪演化成—岛弧。

 
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