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威尔逊旋回
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  wilson cycle
     THE MAFIC-ULTRAMAFIC ROCKS AND WILSON CYCLE
     镁铁-超镁铁岩与威尔逊旋回
短句来源
     Wilson Cycle of the Paleo-Tethyan Orogenic Belt in Western Yunnan:Record of Magmatism and Discussion on Mantle Processes
     滇西古特提斯造山带的威尔逊旋回:岩浆活动记录和深部过程讨论
短句来源
     The Wilson Cycle of the Jinshajiang Paleo-Tethys Ocean, in Western Yunnan and Western Sichuan Provinces
     滇川西部金沙江古特提斯洋的威尔逊旋回
短句来源
     The Okinawa Trough can also be considered as an important link between East African Rift and Red Sea stage in the Wilson Cycle.
     冲绳海槽也可视为是威尔逊旋回中连接东非裂谷和红海阶段的一个重要的中间环节
短句来源
     The paper makes the comprehensive study of the age of the passive continental margin, ophiolites, radiolaria silicalite of ocean basin facies, island arc magmatite and molasses formation of the Jinshajiang Orogenic Belt in Western Yunnan and Western Sichuan Provinces. In the light fossils and SHRIMP dating, it proves the Wilson cycle of the Jinshajiang Paleo-Tethys Ocean, namely, continental cracking (D 3),oceanic spreading(C),oceanic subduction(P) and collision orogency(T).
     本文对滇川西部金沙江造山带被动大陆边缘、蛇绿岩、洋盆相放射虫硅质岩、岛弧岩浆岩和造山磨拉石建造的形成时代进行了综合研究 ,结合古生物化石和 SHRIMP年龄 ,论证了金沙江古特提斯洋盆的威尔逊旋回 ,即大陆裂解 (晚泥盆世 )、洋盆扩张 (石炭纪 )、俯冲消减 (二叠纪 )和碰撞造山 (三叠纪 )。
短句来源
  “威尔逊旋回”译为未确定词的双语例句
     METALLOGENESIS AND WILSON CYCLE-THEIR RELATION?
     矿床与威尔逊旋回——有多少联系?
短句来源
     A small oceanic basin, largest width 800km and similarly late stage of Red Sea and early stage ofAtlantic, is inferred in Changning-Menglian zone from late Devonian to early Carboniferous.
     在D_3—C_1曾有一个小洋盆存在,推断洋盆的最大宽度约为800km,相当于威尔逊旋回红海阶段的晚期或大西洋阶段的早期;
短句来源
     The three types of molasse are genetically related to the models of Welson moun-tain building cycles, on the account of: 1.different types of molasse formed in different stages of Welson cycles;
     上述三类磨拉石与威尔逊造山旋回模式之间有着成因联系,表现为:1.威尔逊旋回的不同阶段形成不同类型的磨拉石;
短句来源
     Study on marginal strutural planes and sections in combination with Wilson cycles, plate movement history, crustal structure, etc.
     根据板缘构造平、剖面特点,结合威尔逊旋回、板块运动史、地壳结构等分析,大陆仰冲板块是在克服属弱对流系一方的洋板块的抵抗,迫使贝尼奥夫带不断向洋退却过程中向前推进.
短句来源
     Since the structural zoning of oceanic subduction stage is the most complex and most obvious according to Welson cycle,so the subduction stage is regarded as the time boundary of division. The first-grade structural unit is lithosphere plate,bounded by ophiolite melange belt of oceanic type.
     按照威尔逊旋回,大洋俯冲阶段的构造分带最复杂、最明显,应该以该阶段作为分区的时间区间,一级构造单元是岩石图板块,以大洋型蛇绿混杂岩带作为分区界线;
短句来源
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  相似匹配句对
     THE MAFIC-ULTRAMAFIC ROCKS AND WILSON CYCLE
     镁铁-超镁铁岩与威尔逊旋回
短句来源
     METALLOGENESIS AND WILSON CYCLE-THEIR RELATION?
     矿床与威尔逊旋回——有多少联系?
短句来源
     Avennue du President Wilson
     威尔逊总统大道
短句来源
     ON THE WILSON DEPRESSION OF THE SUNSPOT
     太阳黑子的威尔逊降落
短句来源
     DISCUSSIONS ABOUT SEQUENCE BOUNDARIES ON CARBONATE PLATFORMS
     层序与旋回
短句来源
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  wilson cycle
The convective geodynamic system of the first rank (GS-1) that functions throughout the mantle and crust beneath the entire surface of the Earth corresponds to the geodynamic cycle of the first rank (GC-1, or the Wilson cycle).
      
The GS-0 is characterized by interference of the permanent westward and meridional (southward and northward, alternately) continental drift in frames of the zeroth geodynamic cycle (GC-0) twice as long as the Wilson cycle (GC-1).
      
The ensialic orogeny in the form of a reduced Wilson cycle that developed under within-plate conditions was the main mechanism of structure formation.
      
Post-orogenic suites mark the end of a post-collision or late orogenic event and the initiation of Pangaea break-up, indicating that a new orogenic Wilson cycle is about to start.
      
The Brasília Orogenic Belt presents features of a Wilson Cycle implying that WMG does not fulfil the geotectonic and geothermometric requisites to host primary diamond sources.
      
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It is indicated in this paper that the mineralization was controlled by the crystallized basement and its shape ,on the basis of the changeable relations and different Pb isotope characters in the three Au, Mo(W) and Pb-Zn ore belts along Qinlin tectonic zone and the distribution regularity of W and Sn deposits in Nanlin area, and the mineralization is not related to the Wilson cycle.

本文以秦岭构造带的金、钼 (钨) 、铅锌3个矿带变化关系,铅同位素不同特点,以及南岭地区钨锡分布规律,说明成矿作用受结晶基底及形态的控制,并非与威尔逊旋回有关。 叙述了威尔逊旋回无法解释世界绿岩带的分布和成矿特点,结合我国华北、华南燕山期成矿特点的地质事实,认为应用威尔逊旋回理论来建立金属矿产的形成、演化模式,不能夸大其它的作用。

Molasse is a sedimentary assemblage which is characteristic of clastic sediments and rapid accumulation on the front of mountain mass. There are three types according to their dynamic backgrounds. divergence(stretching ) type, related to the crustal cracking, 2.convergence ( compressional ) type, related to the collision of lithospheric plates; 3. transformational shearing ) type, related to stretch-rifting basin controlled by strike-slip faults. The three types of molasse are genetically related to the models...

Molasse is a sedimentary assemblage which is characteristic of clastic sediments and rapid accumulation on the front of mountain mass. There are three types according to their dynamic backgrounds. divergence(stretching ) type, related to the crustal cracking, 2.convergence ( compressional ) type, related to the collision of lithospheric plates; 3. transformational shearing ) type, related to stretch-rifting basin controlled by strike-slip faults. The three types of molasse are genetically related to the models of Welson moun-tain building cycles, on the account of: 1.different types of molasse formed in different stages of Welson cycles; 2.each type of molasse has its own peculiarities, due to the differences in dynamics and kinematics of platesj 3.different mineral products formed in different molasses because of the dis-placement and enrichment of the elements in the crust.

磨拉石可定义为以碎屑沉积为特征的、在隆起的山体前缘快速堆积为沉积组合.依其动力学背景,可分为三种类型:1.离散(拉张)型,与陆壳的破裂相关;2.聚敛(挤压)型,与岩石圈板块碰撞相关;3.转换(剪切)型,与受走滑断层控制的拉裂盆地有关。上述三类磨拉石与威尔逊造山旋回模式之间有着成因联系,表现为:1.威尔逊旋回的不同阶段形成不同类型的磨拉石;2.由于板块的动力学和运动学差别,不同的磨拉石有着各自的传殊性;3.由于地壳中元素的迁移和富集,导致不同的磨拉石中形成不同的矿产.

Problems on evolution of plate tectonics in the South and East China Seas are discussed and reviewed in the paper. It is believed that the South China Sea is a basin created by spreading on the basis of passive continental margin, but not a product of back-arc spreading; Taiwan Island is a typical arc-continent collision zone, but not an active arc. The comparison is made between tectonics in areas of Taiwan Island and Himalaya Mountains. The plate boundary from the Luzon to Taiwan Islands exhibits a conversion...

Problems on evolution of plate tectonics in the South and East China Seas are discussed and reviewed in the paper. It is believed that the South China Sea is a basin created by spreading on the basis of passive continental margin, but not a product of back-arc spreading; Taiwan Island is a typical arc-continent collision zone, but not an active arc. The comparison is made between tectonics in areas of Taiwan Island and Himalaya Mountains. The plate boundary from the Luzon to Taiwan Islands exhibits a conversion of subduction into collision, And a general tending from subduction through collision to formation of a new subduction zone during reversion of polarity is shown in the evolution of plate boundary on the east side of the South China Sea, which at last will be a remnant basin surrounded by brocks. The opening and closing of the South China Sea represent a complex form of the Wilson's cycle. It is also believed that the spreading of sea floor with creation of new ocean crust has not appeared yet in the Okinawa Trough, which is a product of back-arc taphrogenesis, but not that of back-arc spreading.

本文就南海、东海及台湾板块构造演化的若干问题展开讨论。我们认为南海海盆是在被动大陆边缘的基础上张开的,而不是弧后扩张的产物;台湾不是活动岛弧,而是典型的岛弧-大陆碰撞带,并将台湾与喜马拉雅地区的构造作了对比;吕宋至台湾的板块边缘显示出板块俯冲至碰撞的转化,南海东缘板块边界演化的基本趋势是,从俯冲到碰撞,进而形成极性相反的新俯冲带,南海海盆终将成为被地块全面包围的残留盆地;南海的开合表现为威尔逊旋回的复杂形式。认为冲绳海槽尚未出现伴有新洋壳形成的海底扩张作用,冲绳海槽是弧后裂陷,而非弧后扩张的产物。

 
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