古太平洋板块,paleo_Pacific Plate
1)paleo_Pacific Plate古太平洋板块
1.It is suggested that the magmatic activity was related to an extension following the subduction of thepaleo_Pacific Plate beneath eastern China.小岭子花岗岩高SiO2、Na2O+K2O、TFeO/MgO,富集轻稀土元素和高场强元素Zr、Nb、Y,低CaO、Ba、Sr,地球化学组成与该区大范围分布的千山花岗岩十分相似,具A型花岗岩特征,其形成与古太平洋板块俯冲至中国大陆东部之下引起的拉张有关。
2)Pacific plate太平洋板块
1.Based on distribution of Mesozoic in East China Sea and magmatic-tectonic events in the eastern Fujian and Zhejiang provinces, Kula-Pacific plate would have relatively strong subduction toward China s mainland during Jurassic-Early Cretaceous, thus East China Sea and the area to the south should be of fore-arc basin.从东海中生界的分布和闽浙东部岩浆构造事件来看,侏罗纪—早白垩世库拉-太平洋板块已对中国大陆有较强的俯冲作用,东海及其以南地区应为弧前盆地性质。
2.Northeastern Asia is geologically composed by North China Block in south, Siberian Block in north and the orogenic belt between them, it was intensively influenced by thePacific plate in Mesozoic-Cenozoic.东北亚地区由南部的华北地块、北部的西伯利亚地块和其间的造山带组成，古生代期间基本完成块体拼贴的造山作用过程，中新生代期间受到东部太平洋板块运动的影响。
英文短句/例句
1.The three granite belts are essentially parallel to the Benioff zone of the Pacific plate against the phitippine Sea plate, with the traction direction opposite to that of the plate movement.三个花岗岩带与太平洋板块和菲律宾板块的毕鸟夫带大致平行。
2.Please tell me the mechanics of how the Pacific Ocean plate moves.请你告诉我太平洋板块怎么运动的机制。
3.Detailed Structure of the Subducting Slab under the Western Pacific Region;西太平洋地区俯冲板块的精细结构研究
4.It was an intraplate earthquake that occurred along the Pacific coast of Chile in South America in 1960.它是1960年沿南美洲智利的太平洋海岸发生的板块间地震。
5.an arm of the Pacific between China and Japan.位于中国和日本之间的太平洋的一块水域。
6.North Pacific Marine Science Organization (PICES)北太平洋海洋科学组织
7.PMEL (Pacific Marine Environmental Laboratory)太平洋海洋环境实验室
8.The Atlantic Ocean is not as big as the Pacific Ocean.大西洋没有太平洋大。
9.Pacific Science Association太平洋科学协会（太科协）
10.Pacific daylight saving time太平洋夏令时太平洋夏令时
11.Pacific satellite太平洋地区卫星太平洋区域通信卫星
12.relating to or bordering the Pacific Ocean.关于太平洋的或太平洋沿岸的。
13.Association scientifique du Pacifique太平洋科学协会（太平洋科协）
14.The Garden of Eden was not in Asia but on a now sunken continent in the Pacific Ocean.现在伊甸园并不是在亚洲，而是在一块太平洋的沉没大陆上。
15.North Pacific Marine Science Organization北太平洋海洋科学组织（海洋科学组织）
16.These are called the Atlantic, Pacific and Indian oceans.它们叫大西洋、太平洋和印度洋。
17.They are called the Atlantic, Pacific and Indian oceans.它们叫大西洋、太平洋及印度洋。00
18.These are called the Atlantic, Pacific, and Indian oceans.它们叫做大西洋，太平洋和印度洋。
相关短句/例句
Pacific plate太平洋板块
1.Based on distribution of Mesozoic in East China Sea and magmatic-tectonic events in the eastern Fujian and Zhejiang provinces, Kula-Pacific plate would have relatively strong subduction toward China s mainland during Jurassic-Early Cretaceous, thus East China Sea and the area to the south should be of fore-arc basin.从东海中生界的分布和闽浙东部岩浆构造事件来看,侏罗纪—早白垩世库拉-太平洋板块已对中国大陆有较强的俯冲作用,东海及其以南地区应为弧前盆地性质。
2.Northeastern Asia is geologically composed by North China Block in south, Siberian Block in north and the orogenic belt between them, it was intensively influenced by thePacific plate in Mesozoic-Cenozoic.东北亚地区由南部的华北地块、北部的西伯利亚地块和其间的造山带组成，古生代期间基本完成块体拼贴的造山作用过程，中新生代期间受到东部太平洋板块运动的影响。
3)West Pacific Plate西太平洋板块
1.The study was focused mainly on the characteristics of earthquake distribution along the collision zone between the west Pacific plate and Eurasian plate, as well as its relation to the form of the west Pacific subduction zone.着重探讨了西太平洋板块与欧亚板块碰撞带的地震分布特征及其与西太平洋俯冲带形态的关系 ,并着重分析了西太平洋板块对欧亚板块地震活动的影响。
4)the subducting Pacific slab太平洋俯冲板块
1.Detailed structure ofthe subducting Pacific slab beneath the Japan islands and Japan sea;日本列岛下太平洋俯冲板块的精细结构
5)Transpacific plate泛太平洋板块
1.Mesozoic volcanism in the eastern part of Northeast ChinaandTranspacific plate;中国东北东部中生代火山活动与泛太平洋板块
6)Underthrust of pacific plate太平洋板块俯冲
延伸阅读
太平洋板块距今1.9亿年前后的印支期，太平洋板块在库拉、法拉隆和特提斯三联点处开始形成[2，3]。以后不断增生扩张，至早白垩世演化为库拉、法拉隆、太平洋和菲尼克斯四大板块。由于库拉—太平洋扩张脊的s—n向增生扩张和太平洋板块南部没有俯冲消减带，便推动库拉板块—太平洋扩张脊以两倍的速度沿横切该扩张脊的s—n向转换断层向nnw快速运动，推挤亚洲板块东北缘并向西潜没于亚洲大陆之下。因此造就了太平洋相对向北、亚洲大陆相对向南的左行直扭应力场，形成了东亚大陆边缘北起苏联远东锡霍特阿林—西南日本—我国东南沿海及台湾—菲律宾的钙碱性安山岩、花岗岩带并与中生界沉积岩、前中生界变质岩一起构成规模宏伟的安第斯式弧形山系。该山系东侧北起西南日本中生代双变质带—济州岛—黄海与东海交界处—东南(浙闽粤)沿海40米等深线处为库拉板块与亚洲板块东缘的转换—敛合边界，其西侧为一系列ne，nne向的褶皱系、左行剪切—挤压断裂体系和山弧后沉积盆地
