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the shanxi formation
相关语句
  山西组
    Discovery of Paratingia and Paratingiostachya from the Shanxi Formation of the Early Early Permian in the Wuda Area of Inner Mongolia, China 
    Paratingia和Paratingiostachya在内蒙古乌达地区早二叠世早期山西组的发现
短句来源
    Sedimentary facies of the Shanxi Formation and Member 8 of Xiashihezi Formation of Permian in Suligemiao area, Ordos Basin
    鄂尔多斯盆地苏里格庙地区二叠系山西组及下石盒子组盒八段沉积相
短句来源
    Research on Controlling Factors of the Shanxi Formation Reservoir in North-east Ordos Basin
    鄂尔多斯盆地东北部山西组储层控制因素分析
短句来源
    The Shanxi Formation consists of sandstones, siltstones, mudstones and coals, with the limestones being locally developed. The thickness of the Shanxi Formation is from 18.6 m to 213.25 m, with the thicknesses of coal seams being from 0 to 10 m and averaging 4.2m.
    山西组以砂岩、粉砂岩、泥岩为主,石灰岩仅在局部地区见到,该组厚18.60-213.25 m,含可采煤层1-2层,厚度0-10.0 m, 平均4.20 m。
短句来源
    The Sedimentary Charcteristcs and Sedimntary Environments of the Shanxi Formation in the Yangquan Coal District, Province Shanxi
    山西阳泉矿区二叠系山西组的沉积特征与沉积环境
短句来源
更多       
  山西组
    Discovery of Paratingia and Paratingiostachya from the Shanxi Formation of the Early Early Permian in the Wuda Area of Inner Mongolia, China 
    Paratingia和Paratingiostachya在内蒙古乌达地区早二叠世早期山西组的发现
短句来源
    Sedimentary facies of the Shanxi Formation and Member 8 of Xiashihezi Formation of Permian in Suligemiao area, Ordos Basin
    鄂尔多斯盆地苏里格庙地区二叠系山西组及下石盒子组盒八段沉积相
短句来源
    Research on Controlling Factors of the Shanxi Formation Reservoir in North-east Ordos Basin
    鄂尔多斯盆地东北部山西组储层控制因素分析
短句来源
    The Shanxi Formation consists of sandstones, siltstones, mudstones and coals, with the limestones being locally developed. The thickness of the Shanxi Formation is from 18.6 m to 213.25 m, with the thicknesses of coal seams being from 0 to 10 m and averaging 4.2m.
    山西组以砂岩、粉砂岩、泥岩为主,石灰岩仅在局部地区见到,该组厚18.60-213.25 m,含可采煤层1-2层,厚度0-10.0 m, 平均4.20 m。
短句来源
    The Sedimentary Charcteristcs and Sedimntary Environments of the Shanxi Formation in the Yangquan Coal District, Province Shanxi
    山西阳泉矿区二叠系山西组的沉积特征与沉积环境
短句来源
更多       
  山西组
    Discovery of Paratingia and Paratingiostachya from the Shanxi Formation of the Early Early Permian in the Wuda Area of Inner Mongolia, China 
    Paratingia和Paratingiostachya在内蒙古乌达地区早二叠世早期山西组的发现
短句来源
    Sedimentary facies of the Shanxi Formation and Member 8 of Xiashihezi Formation of Permian in Suligemiao area, Ordos Basin
    鄂尔多斯盆地苏里格庙地区二叠系山西组及下石盒子组盒八段沉积相
短句来源
    Research on Controlling Factors of the Shanxi Formation Reservoir in North-east Ordos Basin
    鄂尔多斯盆地东北部山西组储层控制因素分析
短句来源
    The Shanxi Formation consists of sandstones, siltstones, mudstones and coals, with the limestones being locally developed. The thickness of the Shanxi Formation is from 18.6 m to 213.25 m, with the thicknesses of coal seams being from 0 to 10 m and averaging 4.2m.
    山西组以砂岩、粉砂岩、泥岩为主,石灰岩仅在局部地区见到,该组厚18.60-213.25 m,含可采煤层1-2层,厚度0-10.0 m, 平均4.20 m。
短句来源
    The Sedimentary Charcteristcs and Sedimntary Environments of the Shanxi Formation in the Yangquan Coal District, Province Shanxi
    山西阳泉矿区二叠系山西组的沉积特征与沉积环境
短句来源
更多       
  “the shanxi formation”译为未确定词的双语例句
    The Carboniferous and Permian Systems in central and south Hebei Pro-vince,remained primarily in some fault-depressed basins and paleosynclines,distri-but within an area of more than 3000km~2 with buried depth of 1500-4600m anda total thickness of more than 1000m,In the Permian System,the ShiqianfengFormation,the Upper and Lower Shihezi Formations are mainly terrestrial clas-tic sediments formed in oxidizing environment,the Shanxi Formation is coal-bearing strata;
    本区石炭、二叠系埋深1500—4600m,主要残留在断陷构造及古向斜中,分布面积3万多平方公里,总厚达1000m 以上。
短句来源
    the littoral delta and the lagoon-tidal flat depositional systems. The coal seam Ⅱ_1 of the Shanxi formation was formed from the lagoon-gulf and the tidal flat subenvironments during the overall regression and the transgression. The variation in thick- ness of coal seam Ⅱ_1 is controlled essentially by the tidal flat subenvironment.
    属泻潮——潮坪及滨海三角洲体系沉积,所含二_1煤层形成于总体海退与短暂海侵的泻湖海湾及潮坪亚环境,其煤厚变化规律主要受潮坪亚环镜所控制.
短句来源
    The minerogenetic series of the Shanxi Formation mainly includes coal beds, followed by expanded clay and siderite.
    山西组成矿系列主要有煤,其次是膨胀粘土矿、菱铁矿。
短句来源
    In the early Early Permian,the epicontinental sea of the North China platform continuously retreated towards south, the Shanxi Formation was deposited a set of mudstone of tidal flat facies in the earlier period and sand mudstone deposits of delta facies dominated the fluviation in the mid late period.
    早二叠世早期,华北地台陆表海不断向南退缩,早期沉积了一套潮坪相泥岩,中、晚期沉积了一套以河流作用为主的三角洲体系。
短句来源
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  the shanxi formation
The thickness of the Shanxi Formation is from 18.6 m to 213.25 m, with the thickness of coal seams from 0.10 to 10 m and averaging 4.2 m.
      
The Shanxi Formation consists of sandstones, siltstones, mudstones, and coals, with the limestones being locally developed.
      


Based on the analysis and study of the characteristics of primarys edimentary structure and its array, lithology, granularity distribution, geochemistry, logging curve, sandbody morphology ard paleocurrent direction, the author has expounded the sedimentary characteristic and sedimentary enviroments of the Shanxi Formation in Yangquan Coal district, built up sedimentary models and made a preliminary study of the characterics of its coal accumulatiou.The present study shows that the Shanxi Formation...

Based on the analysis and study of the characteristics of primarys edimentary structure and its array, lithology, granularity distribution, geochemistry, logging curve, sandbody morphology ard paleocurrent direction, the author has expounded the sedimentary characteristic and sedimentary enviroments of the Shanxi Formation in Yangquan Coal district, built up sedimentary models and made a preliminary study of the characterics of its coal accumulatiou.The present study shows that the Shanxi Formation in this distrct are not "pure continental" as considered by most geologists in the past. It is a set of complex sediment of deltatic system. It went through a process of construction—destruction—construction.

根据对阳泉矿区山西组的原生沉积构造及其组合序列、岩性特征、粒度分布、地球化学、测井曲线、砂体形态及古水流方向等的分析研究,作者阐述了山西组的沉积特征和沉积环境,建立了沉积模式,对聚煤特征作了探讨。研究表明,本区山西组并不是以前大多数地质工作者所认为的“纯陆相”沉积,而是一套复合的三角洲体系沉积。经历了建设—废弃—建设的发展阶段。

The Carboniferous and Permian Systems in central and south Hebei Pro-vince,remained primarily in some fault-depressed basins and paleosynclines,distri-but within an area of more than 3000km~2 with buried depth of 1500-4600m anda total thickness of more than 1000m,In the Permian System,the ShiqianfengFormation,the Upper and Lower Shihezi Formations are mainly terrestrial clas-tic sediments formed in oxidizing environment,the Shanxi Formation is coal-bearing strata;the Benxi and Taiyuan Formations of the...

The Carboniferous and Permian Systems in central and south Hebei Pro-vince,remained primarily in some fault-depressed basins and paleosynclines,distri-but within an area of more than 3000km~2 with buried depth of 1500-4600m anda total thickness of more than 1000m,In the Permian System,the ShiqianfengFormation,the Upper and Lower Shihezi Formations are mainly terrestrial clas-tic sediments formed in oxidizing environment,the Shanxi Formation is coal-bearing strata;the Benxi and Taiyuan Formations of the Middle and Upper carbo-niferous are transitional facies of terrestrial and marine sediments in which theTaiyuan Formation consists of coal measure.The Shanxi Formation contains 4-12 coal beds with a total thickness of8.5-27m;the Taiyuan Formation contains 2-11 coal beds,with a total thick-ness of 2.5-33.5 m.Much carbonaceous and dark mudstones can be found incoal measures.The content of chloroform bitumen“A”is more than 0.2% inthe coal beds,the content of residual organic carbon is generally 0.5-1.0% andchloroform bitumen“A”is 0.048-0.115% in the dark mudstones.Vitrinite reflec-tance of them is greater than 0.5%.These indices show that they are favour-able source rocks.To analyze the hydrocarbon generation of the basin in accordance with tec-togenesis and the conditions of thermoevolution,the Himalayan phase is consi-dered to be an important period,and then the Yanshan phase.The Carboniterous and Permian Systems here have composed a great source-reservoir-cap rock assemblage,which can receive oil and gas from the overlyingEogene too.Thus the assemblage has double oil sources.The trap type on thewhole is considred to be fault-block type.The authors suggest that Wen'an Slop is the most favourable area in oiland gas prospects,and then Shenxian and Langfang ranges;as for the south ofHebei,it is better to seek coal-formed gas.

本区石炭、二叠系埋深1500—4600m,主要残留在断陷构造及古向斜中,分布面积3万多平方公里,总厚达1000m 以上。上石炭统太原组及下二叠统山西组为煤系,有机质丰度高,已成熟,是较好的油气源岩。石炭、二叠系可自成生储盖组合,又可从上覆下第三系中获得油气。从构造运动及热演化条件分析,主要生油气期为喜山期,次为燕山期。文安斜坡的油气远景较好,廊坊地区次之;冀南地区应以找气为主。

The Shanxi formation in the Maling-shan of Dengfeng coal field, Henan shows its development as a deposite of coal bearing sedimentation dominated by transitional phase during the period of marine regression. According to the lithofacies,the lithological characters and the cy- cles of sedimentation,Shanxi formation is separated into four groups and the corresponding strata,Laojuintang sandstone and Fongjiagou sandstone ard now nominated. By means of mineralogy,lithology,palaeontology,geochemistry...

The Shanxi formation in the Maling-shan of Dengfeng coal field, Henan shows its development as a deposite of coal bearing sedimentation dominated by transitional phase during the period of marine regression. According to the lithofacies,the lithological characters and the cy- cles of sedimentation,Shanxi formation is separated into four groups and the corresponding strata,Laojuintang sandstone and Fongjiagou sandstone ard now nominated. By means of mineralogy,lithology,palaeontology,geochemistry and palaeocurrent analysis,facies of sandstone and the coal measures of Shan- xi formation,we come to the conclusion that they are divided into 33 microfacies,four vertical facies sequence and finally into two big depositional systems,i.e.the coastal delta system and the lagoon-wadd barrier-island system.Besides,we found spongilite associated with bra- chiopods in chert limestone or silicious mudstone of coal measure stra- ta.They are much helpful in identifying the sedimentary environment, and as far as we can see they had not been found before in this district. By the research of the regional sedimentary environment and palaeo- structure of coal forming period,we are persuaded that the thickness variationof coal seam Ⅱ_1 was cheafly due to the local sedimentary environ- ment,the differential subsidence of basement and the river erosion,while the tectonic influence in succession played only a minor part. By the analysis of lithofacies-thickness or facies-thickness we con- fessed initially that in the uplift area of this region,coal less than 3.5 meters thick can only be expected,but we can get thick coal of above 8 meters in the depression area in the east and west part of the coal field.

登封煤田马岭山一带,山西组地层是发育在总体海退阶段,以过渡相为主的含煤沉积。据岩性、岩相和旋回结构的研究,首次将山西组地层划分出四个段,并对“老君堂砂岩”和“冯家沟砂岩”提出了命名。据古生物学、矿物学、地球化学、岩石学、古水流、砂岩体及煤层相的研究,用环境参数及相模式法,首次对山西组含煤岩系沉积环境进行系统研究,划分出33个微相,归属为四个垂直相序及泻湖—潮坪—障壁岛和滨海三角洲两大沉积体系。首次在灰岩燧石层、硅质泥层中发现了海绵岩。据沉积环境和聚煤期古构造的研究,初步得出二_1煤厚变化地质因素主要是沉积环境及聚煤期基底差异沉降,其次为河流冲蚀作用及后期构造影响的结论。通过岩相一厚度法或相一厚度分析,初步认为研究区中部隆起区主要为3.5米以下的薄煤带,而大于8米的巨厚煤带则集中分布于研究区东西两侧坳陷区。

 
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