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the shanxi formation
相关语句
  山西组
     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
     DISCOVERY OF THE CATHAYSIOPTERIS WHITEI IN THE SHANXI FORMATION AND ITS STRATIGRAPSHIC SIGNIFICANCE
     怀特华夏羊齿(Cathaysiopteris whitei)在山西组的发现及其地层意义
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
     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
     Obvious suppression in vitrinite reflectance is discovered with strong-reductibility coals(facies I and II )in the Taiyuan Formation(C3 ) as compared with iso-thermally related weak-reductibility coals ( facies III ) in the Shanxi Formation (P11 ) .
     中国华北盆地晚古生代煤系太原组(C_3)强还原型煤(煤相Ⅰ和煤相Ⅱ)与热史相近的山西组(P_1~1)弱还原型煤(煤相Ⅲ)相比,其反射率存在着明显的抑制作用(Suppression)。
短句来源
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  “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
  相似匹配句对
     CHARACEAE OF SHANXI
     山西省的轮藻植物
短句来源
     Shanxi Apartment
     陕西公寓
短句来源
     FOR THE FUTURE OF SHANXI TOURISM
     为了山西旅游的明天——山西旅游职业学院成立专访
短句来源
     THE CULTURE DOOR OF SHANXI
     晋祠:三晋文化的大门
短句来源
     SHIQIANFENG FORMATION OF SHANXI PROVINCE
     山西省的石千峰组
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.
      


Great advances have been achieved in the study of late palaezoic stratigraphy in north China Platform since liberation.They can be summed up as follows. An Early Carboniferous continental-coal-bearing stratigraphy and a Middle Carboniferous Molasse Formation with huge thickness were discovered in the north border of Qinglin-Huaiyang Shield;many marine bivalves fossils from the Shanxi Formation were described by Zhang;the Shiqianfeng Formation might wholly belong to the Lower Triassic in age;...

Great advances have been achieved in the study of late palaezoic stratigraphy in north China Platform since liberation.They can be summed up as follows. An Early Carboniferous continental-coal-bearing stratigraphy and a Middle Carboniferous Molasse Formation with huge thickness were discovered in the north border of Qinglin-Huaiyang Shield;many marine bivalves fossils from the Shanxi Formation were described by Zhang;the Shiqianfeng Formation might wholly belong to the Lower Triassic in age; the age of Shuangquan Formation in the Western Hills of Beijing was confirmed as the Late Permian through a large number of fossil plant study; sufficient evidences showed that the Shanxi Formation and the Lower and Upper Shihezi Formations are far from being pure continental deposits as formerly held, but were formed under the paralic plain enviroment.

解放以来,华北地台晚古生代地层的研究取得了许多新的重大进展:秦岭——淮阳地盾北缘发现了一个早石炭世的陆相含煤地层和一套巨厚的属于中石炭世的磨拉石建造;山西组中发现了许多晚石炭世型的双壳类化石;石千峰组的时代可能全部都有属于早三叠世的可能;根据大量植物化石,北京西山的双泉组的年代肯定是晚二叠世;许多新材料提供的证据都说明山西组和上、下石盒子组均远非以前认为的那样是纯大陆相沉积,而是在滨海平原环境中形成的。

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。

 
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