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facies
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     Early-Stage Description Technique and Its Application of Fluvial Facies Sandstone Gas Reservoir
     河流砂岩气藏早期描述的技术方法及应用
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     The Study of Sedimentary Facies and Analysis of Subtle Reservoir for Taikang--Xichao
     泰康——西超地区沉积研究及隐蔽油气藏形成条件分析
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     The Sequence Stratigraphic Frame Works and Depositional Facies of the Lower Paleozoic in the Northeast of Tarim Basin
     塔里木盆地东北地区下古生界层序格架与沉积研究
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     The Comprehensive Evaluation of Hydrocarbon Preservation Units in Modifying-type Basins of Sea Facies in South China
     中国南方海改造型盆地含油气保存单元综合评价
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     The Research for Distribution and Prediction of Cretaceous and Tertiary Sedimentary Facies and Reservoir Beds in Kuche Depression, Tarim Basin
     塔里木盆地库车坳陷白垩系—第三系沉积及储层分布预测研究
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     Ehlers-Danlos syndrome type VIII: Periodontitis, easy bruising, marfanoid habitus, and distinctive facies
     Ehlers-Danlos综合征Ⅷ型:牙周炎、易擦伤、马方综合征样体型和特征性面容
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  “facies”译为未确定词的双语例句
     Geology, Geochemical Characteristics and Mechanism of Hydrocarbon-generating for Source Rocks from the Tertiary Salty Lacustrine Facies in the West Region of the Qaidam Basin
     柴达木盆地西部第三系咸化湖泊烃源岩地质地球化学特征与生烃机理
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     Sedimentary Facies Analysis of the Middle Carboniferous Series in Fuchowan Region of Province Liao-Ning
     遼寧省复州灣中石炭紀沉積岩相分析
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     ABUNDANCE AND TYPES OF ORGANIC MATTER IN SOURCE ROCKS OF CONTINENTAL FACIES
     陆相生油岩有机质的丰度及类型
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     Exploring reef facies reservoirs in the northern part of the South China Sea
     南海北部海域的礁块勘探
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     TIDAL DEPOSITS OF CARBONATE FACIES AND THEIR MICROFACIES TYPES IN THE QIZIQIAO FORMATION OF MIDDLE DEVONIAN, SOUTH CHINA
     华南中泥盆世棋梓桥组碳酸盐岩潮汐沉积及其微相类型
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  facies
The difference of pressure distribution is caused by the lithologies, facies and faults.
      
The Cangxi reef flat possesses the largest platform edge shallow facies domestically found, and has a typical prograding sequence.
      
Abundant normal alkanes, isoprenoid hydrocarbons, terpanes and steranes were detected in 23 samples taken from the carbonate platform to basin facies in the Devonian Frasnian-Famennian (F-F) transition of Guangxi, South China.
      
A review of lithostratigraphic criteria for subdividing the two adjacent formations provides new regional correlations between the formations and related stratigraphic successions and facies.
      
Pool elements, such as preservation conditions, traps and migration paths, and reservoir rocks and facies, also served as important control factors to marine gas pools in South China.
      
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As a lofty mountain Nanshan stretches along the southern border of Kansu Corridor. In past two decades a few discussions had been given by some sdholars about its landforms and its quaternary glaciations. Based upon my field works and recent reports, we know that there are some close Connections existed between tectonic movements, geomorphic cycles and correlative deposits; and, Consequently, they may be mutually explained. according to the analysis of the facies and distribution of Cenozoic sediments,...

As a lofty mountain Nanshan stretches along the southern border of Kansu Corridor. In past two decades a few discussions had been given by some sdholars about its landforms and its quaternary glaciations. Based upon my field works and recent reports, we know that there are some close Connections existed between tectonic movements, geomorphic cycles and correlative deposits; and, Consequently, they may be mutually explained. according to the analysis of the facies and distribution of Cenozoic sediments, We Know that there a peneplanation developed on the older rocks of Nanshan till pper pliocene, and the red deposits which extended over the Nansban and its adjacent regions Were laden down in the same time. Probably laterly, a crusalt movement, which included mul iple uplifts, initiated. The present geomorphic features of Nanshan are possibly resulted from them. as the dissected summit-levels, the remnants of old peneplains Can be found on many mountain tops today. As regards quaternary glaciations of Nanshan, a more important sign ification should be ascribed to the uplifts of this mountain. Perhaps boh because of the uplifts and the Climatic changs, in Nanshan two glacio pluvial periods had occured in quaternary. When the glaciers expanded all of the mountain peaks and valleys. Later on, the glacio fluvial waters were Carrying much debris and forming sedimentary units, which have been called inland molasse formation, into piedmont plain. a distinct interval, which indicat a true interglacial stage, have been found in that formation. The following table shows the main geological changes of Cenozoic of Nanshan.

河西走廊之南延伸着雄伟的祁连山,在过去20年中一些学者曾对该山的地貌和其第四纪冰期作过一些探讨。根据本人的野外工作及最近的文献资料,我们看到,在构造运动、地貌循环和相关沉积三者之间有着紧密的联系,因而,它们可以相互解释。分析岩相和新生代沉积的分布,我们得知直到上上新世,祁连山进行着准平原化的过程,同时并沉积下红色沉积,它遍及祁连山内外。后来,地壳运动开始,它包括多次上升。现代的祁连山的面貌即是多次上升的产物。古准平原的遗跡,目前可在许多山顶发现。祁连山的第四纪冰期的发生,山地上升占有重要地位,可能正是由于上升和气候变化的同时作用,祁连山发生两次冰期——多雨时期。当时冰川遍及山峰和谷地,稍后,冰融水携带大量碎屑物质带入山足平原形成内陆磨拉石建造的沉积。在该沉积岩系中发现有一清楚的间断,这代表一次真正的间冰期。祁连山新生代的主要地质事件见84页附表。

The tectonic movements of the compound platform in Eastern China have deep effects upon the coal formations.Due to tectonic control, the distribution of coal basins in the Mesozoic Era, the limitation of rock facies in the coal formations and the magmatic activity effecting the quality of coal, all appear to follow certain laws of regularity.Types of formations in this era, present more varieties than those of the Paleozoic, in general, faulted depressions are most common. The whole history of coalification...

The tectonic movements of the compound platform in Eastern China have deep effects upon the coal formations.Due to tectonic control, the distribution of coal basins in the Mesozoic Era, the limitation of rock facies in the coal formations and the magmatic activity effecting the quality of coal, all appear to follow certain laws of regularity.Types of formations in this era, present more varieties than those of the Paleozoic, in general, faulted depressions are most common. The whole history of coalification showed that the crustal movement was not regular and the difference in the degree of subsidence also effect the depositional environments. All the above facts are believed to be the direct causes for the frequent change of space in the process of coalification; while the effect of climate seems to be of minor importance.The general occurrence of folding and block-movement in the Mesozoic constantly helps in promoting the topographic changes of the continetal area. Landforms are becoming more complicated. Different paleogeographic environments present different coal formations, thus resulting great many types of paleogeography regarding coalification.Types of coal-bearing rock series are not only of alternating marine and continental origin, but also include all kinds of typical continental sediments. The rock nature and facies as well as the coal-bearing condition of each type, all have their special characteristics.

中国东部地台的构造运动对含煤建造具有深刻的影响. 由于构造的控造,中生代聚煤盆地的分布,含煤建造的岩相控制、岩浆活动对煤质的影响均有显著的规律性.建造类型较古生代多样化,一般以断裂凹陷型为最普遍.整个聚煤历史表明由于地壳运动不均一、沉降幅度不同等因素影响了沉积环境,从而使聚煤作用发生空间方面迁移的现象,而气候影响则为次要的因素. 中生代广泛的折皱和块断运动不断加深了大陆地形的变化,地貌景观益加复杂,不同的古地理环境形成不同的含煤建造,因而聚煤古地理类型繁多.中生代含煤岩系既具有海陆交替相沉积也有各式各样的陆相沉积,每一类型的岩性、岩相及含煤性均有各自的特点.

Gondwana facies of Late Carboniferous and Permian age have been widely distributed in the Qomolangma Feng region in Southern Xizang, China. This paper describes the sediments in the northern slope of the Qomolangma Feng recently discovered by the Qomolangma Feng Scientific Expedition during the years 1974-1975, and also roughly correlates them with the sediments of Salt Range and other regions of the Himalayas.The Gondwana facies concerned here are characterized by the glacial marine sediments, the...

Gondwana facies of Late Carboniferous and Permian age have been widely distributed in the Qomolangma Feng region in Southern Xizang, China. This paper describes the sediments in the northern slope of the Qomolangma Feng recently discovered by the Qomolangma Feng Scientific Expedition during the years 1974-1975, and also roughly correlates them with the sediments of Salt Range and other regions of the Himalayas.The Gondwana facies concerned here are characterized by the glacial marine sediments, the Stepanoviella fauna of Jilong Formation and the Glossopteris flora of the Qubu Formation. The Jilong Formation with thickness about 730 m, can be subdivided into the lower Zhadari diamictite member, the middle Stepanoviella arenaceous siltstone member and the upper Chaya Quartzose sandstone member. The Zhadari diamictite member, thick approximately 30 m, consists mainly of grey diamicti-tes of glacial marine origin and may be correlated with the Talehir boulder beds from the Indian sub-continent, the age of which is generally believed to represent Late Carboniferous or Late Carboniferous to Early Sakmarian stage. The Stepanoviella arenaceous silttone member, about 0.5-1m thick, consists of bioclastic arenaceous siltstone with aboundent megafossils known as Stepanoviella fauna of Late Sakmarian to Early Artinskian stage, comparable with the Umaria marine beds or Eurydesma fauna (s.l.) from the Indian sub-continent. The chaya quartzose sandstone member, about 700 m thick, consists of the fine sandstone and quartzose sandstone intercalated with some shales. The Qubu Formation (about 20m thick) is represented by quartzitic sandstone and shales of early Late Permian, very rich in Glossopteris flora and comparable with Raniganj Formation of the Damuda, Group in the Indian sub-continent.Following the plate tectonics theory, the "Xiang Quan-Yalu Tsangpo suture" probably represents the collision boundary of the Indian Plate subducted beneath the Eurasia Plate before 70-12 million years. Thus it obvious that the whole Himalayan mountains once occurred as a part of the northern margin of the Indian Plate, as is shown by the occurrence of the Gondwana facies in the northern slope of the Qomolangma Feng and other regions of the Himalayas. It is, therefore, suggested that the Southern Tethyan Himalayan Sea in Late Palaeozoic was an epiric sea associated with the Indian Plate.From the informations mentioned above the northern boundary of the Gondwana facies occurred in Asia continent seems to be not beyond the Xiang Quan-Yalu tsangpo river geosuture.

于1975年我国再次登上珠穆朗玛峰的科学考察活动中,在地质方面获得了地层、古生物、岩石、构造等方面比较珍贵的资料。珠峰科考资料研究的新成果是在反击右倾翻案风斗争取得伟大胜利的大好形势推动下取得的。本刊将发表《珠穆朗玛峰北坡冈瓦纳相地层的发现》等相互联系的一组文章,从地层、沉积、古生物的角度,以较丰富的资料证实了珠峰北坡冈瓦纳相地层的存在,这对于探讨珠穆朗玛峰及喜马拉雅山的隆起和地质发展史具有重要价值。

 
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