Chinese translation for "板块碰撞"

collision of plates
plate collision

Related Translations:

板块:  [地] plate◇板块边缘 plate margin; 板块构造 plate tectonics; raft tectonics; 板块假说 plate hypothesis; 板块碰撞 plate collision; 板块学说 plate tectonics; 板块运动 plate motion; plate movement

小板块:  microplatesmall platesmallplate

板块运动学:  plate kinematicsplate kinetics

板块厚度:  plate thickness

俯冲板块:  diving slabdowngoing slabsubductingplatesubduction plateunderthrust plate

旋转板块:  rotated plate

板块挤压:  plate jamsplate-jam

地质板块:  plate

凹板块:  concave

板块增长:  creation of plate

Example Sentences:

	1.	When an ocean plate bumps into a land plate , the less dense land plate floats over the ocean one 当大洋板块与大陆板块碰撞时，稍薄的大陆板块就会漂在大洋板块之上。
	2.	The middle proterozoic granitoids was an intraplate type producted in transitinal crystalline basement before plate collision 中元古界的花岗岩类是板块碰撞前过渡性结晶基底上局部熔融花岗岩类。
	3.	The sinian granitoids are immediately related the plate collision , they were formed in the plate collision mounain - building period - post collision elevation period 震旦纪花岗岩类与板块碰撞作用密切有关，是碰撞造山一碰撞后抬升这一过程形成的花岗岩类。
	4.	It is the only protected area in the world to incorporate a continuous , intact transect from snowcap to tropical marine environment , including extensive lowland wetlands 它位于两个大陆板块碰撞的地方，这里的地质情况很复杂，既有山脉的形成又有冰河作用。
	5.	After growing to a certain height , the effect of gravity and collision - generated extrusion will make them grow wider , but not higher , bian said 边教授说，喜马拉雅山达到一定高度后，在重力和由板块碰撞产生的挤压力的作用下，山脉会向外扩展，而不会持续增高。
	6.	To benzilan ( where visitors can view the geological legacy of the collision of the european - asian plate with the indian sea plate ) , then on to the dongzhu temple group , and then proceeding to baimang snow - capped mountain , and the feilai temple in deqin , and on to meili snow - capped mountain , mingyongqia glacier , and xidang hot springs from which one can continue on to the yuben fairy waterfall 由中甸为起点，松赞林寺、纳帕海、奔子栏（游览欧亚板块与印度洋板块碰撞地质遗址） 、东竹林寺、白茫雪山、德钦飞来寺、梅里雪山、明永恰冰川、西当温泉、雨崩神瀑。
	7.	Tian shan extends east - west in central asia , the tian shan range was formed in later paleozoic , and a few intramontan basins appeared in mesozoic . it uplifetd again in early miocene because of the north - south compression induced by the india - asia collision , so many active structures can be found in tian shan . active tectonics took actions during last ten thousands yeas , and surface traces of fault scarps , detached gullies and folds in alluvial deposit are apparent , so it is easy to distinguish them from other geological phenomema 天山位于亚洲中部，天山造山带形成于晚古生代，到中生代时，在天山内部形成了一些山间盆地，印度板块在始新世向北与欧亚板块碰撞，天山受南北向挤压力的作用再度于早中新世隆起，由于板块碰撞的持续进行，在天山山间及山前发育了许多的活动构造。
	8.	( 6 ) the geological significance of oblique - thrusting fault of sertengshan - xitieshan was discussed in this paper . the oblique - thrusting effect of sertengshan - xitieshan is the result of the long distance effction of himalayan orogenic belt intracontinent subducting , which is of great theory significance for studying regional structural framwork , relations between basins and mountains and oblique - thrusting effect of large - scale fault zone or orogen in northern qaidam basin . moreover , the result is of guidance significance for the forecast of combination gas , distributing and formation of nappe metal deposit in northern qaidam basin ( 6 )论文探讨了赛什腾? ?锡铁山斜向逆冲推覆构造的地质意义，认为赛什腾-锡铁山断裂斜冲作用是印度板块与欧亚板块碰撞、会聚的远程效应的结果，该认识对于研究柴北缘区域构造格局、盆山关系以及更大尺度的断裂带或造山带的斜向逆冲作用具有理论意义，对柴达木北缘的油气预测、推覆体金属矿床的分布、形成具有指导意义。
	9.	The three orogenic belts of sanjiang , qinling and xingan - mongolia developed in china from south to north , not only record the perfect history of the paleo - asia plates evolutionary process , and also reflect the effects of pacific plate subducting and indian - asia continent collision on continental margin and intern , especially these orogenic belts have experienced the main processes and metallogeny during the collision to post - collision and 我国从南往北发育的三江造山带、秦岭造山带和兴蒙造山带，记录了古板块演化旋回及其成矿作用的完整历史，也叠加了中新生代太平洋板块俯冲和印度板块碰撞导致的大陆边缘及陆内效应的信息。
	10.	And apatite . by these analyses and comparison with general granite both in china and the world and with the granite in other au or cu belt in china , the characteristics of the granite in this area are concluded as follows . it belongs to magnetite - i or syntectic granite and has crust - mantle mixed characteristics ; it was formed mainly by crystallization differentiation of melting magma and multiphase varied intrusion ; the degree of differentiation evolvement is not high ; the granite and its enclaves p . re congenetic ; the range of temperature is about 500 - 700 , the range of pressure is about 2 . 50 gpa - 4 . 35 gpa , and the range of oxygen fugacity ( lg fo2 ) is - 15 . 53 - - 14 . 00 ; most granite bodies formed before the collision of plates , and few formed after the collision of plates 通过对测试数据的分析与综合研究，并同中国和世界一般花岗岩类以及中国主要金、铜成矿岩体的花岗岩类进行对比，得出本区花岗岩类岩石具有以下特征：属磁铁矿-型或同熔型花岗岩，其岩浆物质具壳幔混源特征：主要由熔融态岩浆经结晶分异作用，通过多期变速上侵而形成；其分异演化程度较低；寄主岩基和包体具有同源性；岩石的形成温度范围约为500 - 700 ，压力大约为2 . 50gpa - 4 . 35gpa ，氧逸度值1gfo _ 2为- 15 . 53 ? 14 . 00 ；该岩带主要形成于板块碰撞前消减的活动板块边缘期，为燕山至喜马拉雅早期的大陆边缘火山弧环境的产物。

Similar Words：

"板块内部地震" Chinese translation, "板块内部玄武岩" Chinese translation, "板块内的" Chinese translation, "板块内的；内陆板块" Chinese translation, "板块内地震" Chinese translation, "板块碰撞带" Chinese translation, "板块碰撞作用" Chinese translation, "板块驱动力" Chinese translation, "板块三结合点" Chinese translation, "板块绳状熔岩" Chinese translation