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   威尔逊旋回 在 地质学 分类中 的翻译结果: 查询用时:0.022秒
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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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  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.

The study of nappe tectonics is of quite important theoretical and practical significance.

推覆构造的研究具有重要的理论和实际意义,经过对推覆构造形成的地球动力学机制进行的探讨,提出了层圈运动是地球本身运动的基本形式;层圈运动的动力来源于物质横向上的分布不均,层圈运动的必然结果是出现推覆构造体系。根据该理论,推覆构造仅仅发生于不同大地构造单元的界线附近;推覆构造的形成机制是下俯作用。从而对大陆的发生、发展及消亡提出新的见解,把用于洋壳的威尔逊旋回发展到陆壳上,提出了新的全球大地构造旋回。该文在此基础上提出了推覆构造体系这一构造模式。

 
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