西伯利亚板块

西伯利亚板块旋转漂移运动刍议

A Personal View on Rotation Drift Movement of the Siberia Plate

西伯利亚板块与哈萨克斯坦板块间的缝合线在达尔布特-克拉麦里。

The suture of Siberia plate and Kazakstan plate goes along Darbut-Kelameili .

新疆西准噶尔地区位于西伯利亚板块与准噶尔板块的碰撞带。

Western Zhunge'er of Xinjiang lies at the collision belt between Siberia and Zhunge'er plate .

西伯利亚板块是世界上古老的地质构造单元之一。

The Siberia plate is one of the old geological structure units in the world .

诺尔特地区位于阿尔泰北部山区，西伯利亚板块西南缘。

The Nurt area is located in the north of Altay , at the southwest of the Siberia plate .

在1.0Ga左右，由西伯利亚板块和华北板块对接碰撞，形成了巨大陆缘碰撞造山带。

This significant tectonic belt was formed by the collision between Siberia plate and North China plate in about 1.0 Ga.

内蒙古东北部地处西伯利亚板块南缘，南与中朝板块相邻。

The northeast of Nei Mongol is located in the fringe of the Siberia plate and adjacent to the Sino Korean plate .

晚石炭世早期准噶尔盆地可能已经成为西伯利亚板块南缘的一部分。

The Junggar basin might have become a part of the southern margin of thee Siberian plate in the early stage of Late Carboniferous .

早石炭世末，准噶尔-哈萨克斯坦与西伯利亚板块发生陆-陆碰撞，形成大型双重逆冲推覆构造。

The continental collision between Siberian and Kazakhstan-Junggar in Early Carboniferous shaped the large-scale dual thrust-nappe structures in the Altay orogen , NW China .

诺尔特地区位于北阿尔泰构造带的东部，西伯利亚板块西南缘。

The Nurt area is located in the east of the northern Altay tectonic zone , at the southwest edge of the Siberia plate .

岩浆作用产生在西伯利亚板块和准噶尔板块碰撞后开始拉张环境，继承了岛弧岩浆作用的特征。

It was formed in an extensional environment developed after the collision between Siberia and Junggar continental plates , inheriting the features of island-arc magmatism .

大青山东段位于内蒙古中部，华北地台北缘，属于西伯利亚板块与华北板块碰撞带范畴。

The eastern segment of Daqingshan is located in the middle part of Inner Mongolia , China and in the northern margin of North China platform .

查干诺尔铜矿床产在西伯利亚板块和华北板块汇聚带附近，华力西晚期构造岩浆带内。

The Chaganuoer copper deposit is located near the assembly belt of Siberian plate and North China plate , and within the tectonic-magma belt of Late Variscan .

本文还从电性结构特征探讨了西拉木伦河断裂带可能是西伯利亚板块和中国板块的缝合线。

According to the geoeletrical structure it is supposed that the Siramulen River fault zone seems to be a tectonic suture line between Siberia plate and China plate .

研究区位于西伯利亚板块东南大陆边缘晚古生代陆缘增生带，是古亚洲成矿域的重要组成部分。

The survey region , an important part of Palaeo-Asia metallogenic domain , is located in the Late Paleozoic terrigenous hyperplasia belt of southeast continental margin of the Siberian plate .

其动力机制为印度板块向北推移、西伯利亚板块向南运移发生对挤，脆&韧性剪切变形导致了井田现有的构造组合形式。

The structural dynamic mechanism is compressing northward Indian Plate and southward Siberian Plate caused brittle-ductile shearing deformation in upper crust , thus the minefield structural assemblage forms were formed .

和西伯利亚板块刚性体外围的岛弧体系经构造软碰撞拼合而成，它们又经历了块体拼合后的构造-岩浆热事件（如基性岩浆底侵作用）的进一步改造和影响。

And Siberia plate that occurred in different stages of the Paleozoic and subsequently experienced Mesozoic modification by tectonic_magmatic thermal events ( such as the basic magmatic basal erosion ) .

结合前人厘定的板块俯冲时间（408~376Ma），推测西伯利亚板块与哈萨克斯坦&准噶尔板块的碰撞时限为376~334Ma。

In combination with the previously assumed plate subduction time ( 408-376 Ma ), the collision of Siberian Plate with Kazakstan-Junggar Plate can be limited within the range of 376-334 Ma .

区域构造研究结果表明，形成的构造背景与古亚洲洋的消减，西伯利亚板块与中朝板块碰撞对接作用派生的剪切作用有关。

Studies on the regional tectonics show that the tectonic setting is related with the consuming of the Paleo Asia ocean , with the colliding and connecting of Siberian plate with Sino Korean plate .

黑龙江伊春延寿成矿带隶属于小兴安岭张广才岭成矿带，后者位于西伯利亚板块（东南缘）与布列亚佳木斯板块两大板块的缝合带。

Yichun – Yanshou geosynclinal fold system is a part of Xiaoxing ' anling - Zhangguangcai metallogenic belt , which belongs to the suture of Siberian plate ( southeAst edge ) and bureya - Jiamusi plate .

根据岩石化学和微量元素特征及有关判别图，都山等印支期花岗岩可能属中朝板块与西伯利亚板块碰撞造山作用的后碰撞花岗岩。

Based on petrochemistry , trace element characteristics and the discrimination diagrams , the studied Indosinian granites , such as the Dushan granite are likely to be generated by the post collision between the Sino Korean plate and the Siberia plate .

复向斜的形成机制完全符合纵弯褶皱作用下岩石的变形原理，是西伯利亚板块和华北板块碰撞的结果；秦皇岛背形的形成是后期太平洋板块俯冲在欧亚板块之下所致。

Mechanism of the synclinorium is completely coincided with the rock deformation under the longitudinal bending and the synclinorium is resulted from collision of the north China plate and Siberia plate and Qinhuangdao antiform from the subduction of pacific plate under Eurasian plate .

本文试从展现板块的水平运动特点出发，着重揭示西伯利亚板块在各地质时期的运动状态，从而阐述该板块自寒武纪以来的旋转漂移的全过程。

In view of the characteriatics of level movement of the plate , this paper reveals mainly the moverment state in geological periods of the Siberia plate and deals with the total processes of rotation drift movement of the plate since the Cambrian period .

中侏罗世早白垩世中期形成的辽西地区道冲推覆构造系既与西伯利亚板块与华北板块之间蒙古鄂霍茨克大洋最终闭合碰撞有关，同时也与古太平洋板块向西俯冲在东亚大陆之下有关。

The formation of the Middle Jurassic-middle Early Cretaceous thrust nappe system in western Liaoning was related to the final closing of the Mongolian-Okhotsk Ocean between the Siberian and North China plates and plate collision and westward subduction of the Paleo-Pacific plate beneath the East Asian continent .

位于西伯利亚板块阿尔泰大陆边缘的克兰泥盆纪火山沉积盆地具有明显的非对称性，其沉积构造演化经历了三个阶段：早期酸性火山-沉积阶段、中期基性火山-沉积阶段、晚期碎屑沉积阶段。

Located in the Altay edge of the Siberia plate , the Kelan Basin is obviously an asymmetric Devonian volcano-sedimentary basin , its sediment-structural evolution may be divided into three stages : the early acidic volcano-sedimentary stage , the middle base volcano-sedimentary stage and the late clastic sedimentary stage .

在全球构造演化中，古生代它们被夹持于周围巨大的大洋板块之间，中生代以来则夹持于同样巨大的西伯利亚、印度大陆板块和太平洋诸大洋板块之间。

In the global tectonic evolution , they were placed in between the surrounding macro-oceanic plates in Palaeozoic , and in between the Siberian and Indian continental plates and several oceanic plates in Pacific since Mesozoic .