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非威尔逊旋回
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  “非威尔逊旋回”译为未确定词的双语例句
     Problems (Issues), which are paid close attention to in the research of continental dynamics, such as the classical, unclassical and un-Wilson's-Cycle during the continental dispersion (or splitting) and collision;
     本文对大陆动力学研究中密切关注的问题,如大陆裂解和碰撞的经典、非经典、非威尔逊旋回
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  相似匹配句对
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     论威尔逊的全球主义
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     典后遗症?
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     广义布尔
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Problems (Issues), which are paid close attention to in the research of continental dynamics, such as the classical, unclassical and un-Wilson's-Cycle during the continental dispersion (or splitting) and collision; the multi-variety and polyphose of basin-mountain transformation; the vertical and flank accretion of continents by olelamination or “Choula” (drawing ) ?; the complex and various structure of orgenic belt; and the “dynamic source”of development and evolution of the continental lithosphere have been...

Problems (Issues), which are paid close attention to in the research of continental dynamics, such as the classical, unclassical and un-Wilson's-Cycle during the continental dispersion (or splitting) and collision; the multi-variety and polyphose of basin-mountain transformation; the vertical and flank accretion of continents by olelamination or “Choula” (drawing ) ?; the complex and various structure of orgenic belt; and the “dynamic source”of development and evolution of the continental lithosphere have been discussed and analysed. At the some time, ideals on the above problems (issues) have been put forward.

本文对大陆动力学研究中密切关注的问题,如大陆裂解和碰撞的经典、非经典、非威尔逊旋回;盆─山转换的多类型多阶段;大陆垂向增生与侧向增生──是拆沉还是抽拉?造山带结构的复杂性和多样性以及大陆岩石圈发展与演化的“力源”等问题进行了归纳分析和讨论,同时提出了笔者对上述问题的看法。

The Central Orogenic Belt originally consisted of a series of microplates plus two rows of micro_oceans of different stages located respectively to the south and north of the microplates. Qaidam, Qinling, Dabie-Sulu (Jiangsu-Shangdong) plus central Qilian constitute the main body of the microplates. During end_Proterozoic and early Early Paleozoic, the northern row extended into archipelagic oceans, which closed by the end of Caledonian stage and formed foreland basins along the northern margin of the microplates....

The Central Orogenic Belt originally consisted of a series of microplates plus two rows of micro_oceans of different stages located respectively to the south and north of the microplates. Qaidam, Qinling, Dabie-Sulu (Jiangsu-Shangdong) plus central Qilian constitute the main body of the microplates. During end_Proterozoic and early Early Paleozoic, the northern row extended into archipelagic oceans, which closed by the end of Caledonian stage and formed foreland basins along the northern margin of the microplates. Meanwhile the southern row formed rift valleys which closed simultaneously but did not transform into mountains. The microplates incorporated with Eurasia in Late Paleozoic and shifted northward with it. The southern row developed into Late Devonian (individually), Carboniferous-Permian micro_oceans belonging to parts of Paleo_Tethys. They closed during Middle-Late Permian and formed Early-Middle Triassic foreland deposits to their south. During the Indosinian stage this belt belonged to the northern branch of Paleo_Tethys, and the Triassic consisted of three types. The Yanshanian intracratonic compression strengthened eastward, causing maximum subduction and topographic uplift of the eastern microplates. Such effects decreased westwards. Plate tectonics of the Central Orogenic Belt ensues mainly the Non_Wilson Cycle rather than the Wilson Cycle. The Non_Wilson Cycle differs from the Wilson Cycle in three aspects, i.e., archipelagic ocean, soft collision and multicyclicity. This paper discusses their characteristics, and emphasizes that the Non_Wilson Cycle with its three aspects is of general significance in the development of Paleo_Asian and Tethys Oceans which occupied the main territory of China in geological history.

中央造山带原型是由一列微板块加上分别位于其北面和南面的两列不同时期的小洋盆组成.微板块群的主体是柴达木、秦岭、大别—苏鲁,还加上中祁连.元古代末至早古生代早期,北列拉张成多岛小洋盆,它们在加里东末期关闭,并在微板块群北缘形成前陆盆地带.南列形成裂陷槽,在加里东期末关闭,一般不造山.晚古生代,微板块群已与欧亚板块合为一体,并总体北移.南列出现泥盆(个别)、石炭二叠纪的小洋盆,属于古特提斯洋的一部分.洋盆在中—晚二叠世闭合,在其南侧形成早—中三叠世的前陆堆积.印支期它属于特提斯北支.三叠系可分成3种类型.燕山期的陆内挤压东强西弱,使东部微板块消减最多而抬升最高,向西依次递减.中央造山带的板块运动主要遵循的不是威尔逊旋回,而是非威尔逊旋回非威尔逊旋回在3个方面与威尔逊旋回不同,即多岛洋、软碰撞和多旋回造山.文中论述了它们的特点,并强调指出这些特点在地史上占据中国绝大部分地区的古亚洲洋和特提斯洋中具有普遍性.

The authors find out Su Jiao Orogenic Belt is a composite orogenic belt formed by the multimechanism orogenesis according to the research of orogenic system of Su Jiao Orogenic Belt in Jiangsu section. It underwent Miocene Proterozoic Wilson Cycle which belonged to the composition of super continental reconstruction and the post occurred reorogenesis of non Wilson Cycle during Triassic period. It is a mainly intracontinental ramp orogenic belt...

The authors find out Su Jiao Orogenic Belt is a composite orogenic belt formed by the multimechanism orogenesis according to the research of orogenic system of Su Jiao Orogenic Belt in Jiangsu section. It underwent Miocene Proterozoic Wilson Cycle which belonged to the composition of super continental reconstruction and the post occurred reorogenesis of non Wilson Cycle during Triassic period. It is a mainly intracontinental ramp orogenic belt formed by Triassic reorogenesis. After the emergence of Wilson and non Wilson Orogenic Cycle, there occurred a large scale isostatic elevation, magmatic activities and basin building orogenesis of upper crust in the mountain chain of SU Jiao Orogenic Belt because of the snapping down in the root of mountain. The study of the ese characters over mentioned have some universal significance. Belt because of the snapping down in the root of mountain. The study of these characters over mentioned have some universal. Significance for the understanding of the Central Orogenic System and continental orogenic belts in the world.

苏胶造山带是多机制造山作用形成的复合造山带 ,它经历了中新元古代威尔逊旋回之后 ,于三叠纪发生了非威尔逊旋回的再造山作用。它主要是三叠纪再造山作用形成的陆内对冲造山带。并且 ,苏胶造山带在威尔逊旋回和非威尔逊旋回之后 ,由于山根拆沉 ,山脉均出现大规模均衡抬升、岩浆活动和上地壳的造盆成山作用。苏胶造山带的上述特征在中央山系及全球大陆造山带中具有一定的普遍意义。

 
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