助手标题  
全文文献 工具书 数字 学术定义 翻译助手 学术趋势 更多
查询帮助
意见反馈
   the upwelling mantle 的翻译结果: 查询用时:0.19秒
图标索引 在分类学科中查询
所有学科
地质学
更多类别查询

图标索引 历史查询
 

the upwelling mantle
相关语句
  “the upwelling mantle”译为未确定词的双语例句
     (3) the detachment structure is the channel of the upwelling mantle fluids;
     碱交代岩是地幔流体转变为热液的化石记录; (3)拆离断层构造体系是地幔流体上升到地壳后的活动通道;
短句来源
     This paper discusses the spatial distribution of the Emeishan Large Igneous Province on the basis of the upwelling mantle plume-crustal uplift model and estimates the scale of Emeishan LIP.
     根据上升地幔柱地表抬升模型对峨眉山大火成岩省空间展布进行了讨论,并推算出该大火成岩省的规模。
短句来源
     The upwelling mantle flow originates from the core-mantle boundary and is mainly manifested in the lower mantle and lower part of the upper mantle. At the top of the upper mantle and at the surface, its location coincides with that of modern hot spots.
     地幔上升流起源于核幔边界,主要表现在下地幔和上地幔下部,到上地幔顶部和地表与现代热点位置符合。
短句来源
     The Linzizong volcanism in southern Tibet correlates the upwelling mantle flow prior to the India-Asia collision or during the early stage of the collision.
     南部的林子宗火山区对应了印度板块与欧亚大陆碰撞前或碰撞早期高原下的地幔上升流.
短句来源
  相似匹配句对
     Upwelling east of Hainan Island
     海南岛东部上升流研究
     the upwelling dominates in the southern SCS;
     南海南部,基本上被上升流海域所控制.
短句来源
     Numerical Method of Coastal Upwelling
     沿岸上升流数值模拟
短句来源
     ON THE RELATIONSHIP OF THE UPWELLING WITH FISHERY OFF ZHEJIANG
     浙江近海沿岸上升流与渔场的关系
短句来源
     EFFECTS OF MANTLE UPWELLING ON POTENTIAL EARTHQUAKE FRACTURE
     地幔物质上涌对地震断裂酝育的作用
短句来源
查询“the upwelling mantle”译词为用户自定义的双语例句

    我想查看译文中含有:的双语例句
例句
为了更好的帮助您理解掌握查询词或其译词在地道英语中的实际用法,我们为您准备了出自英文原文的大量英语例句,供您参考。
  the upwelling mantle
This is probably linked to the upwelling mantle plume imaged beneath the Massif Central (Granet et al.
      
Fractional melting of the upwelling mantle diapirs forms new crust in the backarc basins, the island arcs, and part of the forearc.
      


On the basis of aeromagnetic data the Curie depth over the Bohai Sea water area was calculated by using the method of spectral analysis of residual anomalies described by Prof. B. K. Bhattacharyya. The results obtained indicate that the crustal temperature under the sea is rather higher and in some places the Curie point is located only at a depth of 12km.The idea that the Bohai Sea area can be viewed as a high point for upwelling of materials in upper mantle beneath the North China region was formulated...

On the basis of aeromagnetic data the Curie depth over the Bohai Sea water area was calculated by using the method of spectral analysis of residual anomalies described by Prof. B. K. Bhattacharyya. The results obtained indicate that the crustal temperature under the sea is rather higher and in some places the Curie point is located only at a depth of 12km.The idea that the Bohai Sea area can be viewed as a high point for upwelling of materials in upper mantle beneath the North China region was formulated by many researchers in geoscience according to the geological and geophysical data from the Bohai Sea and the surrounding areas. And later it was confirmed to be correct by the calculated results mentioned above. Therefore, the high heat values that appeared in the Bohai depression and the surroundings are not occasional but have a deep-seated background. Thus the upper mantle u'pwarping from the North China block fault, leading to thinning out of crust and subsiding and squeezing of heated materials into crust along the faults, all promoted the thermal action, in which the Tancheng-Lujiang fault zone would play a specially important role. The upwelling mantle materials through this fault zone resulted in a gradual increase (from west to east) of the temperature field in the North China region and reached its maxium over the Bohai Sea area.This paper indicates that the earthquakes having occurred in the North China region including the Bohai Sea area cannot be fairly explained simply by the stress field formed in collision of some lithospheric plates around the Chinese mainland. The horizontal gradient of temperature field generated during the upward flow of deep-seated heat materials due to the non-homogeneity of earth crust is closely related to the seismicity in the North China region.

本文用航磁资料根据B.K.Bhattacharyya教授提出的剩余异常谱分析的方法,计算了渤海水域的居里面。结果表明,渤海水域下面,地壳温度很高,有些地方居里等温面的深度只有12公里。这说明,许多学者根据渤海及周围地区的地质及地球物理资料,推测渤海是华北地区上地幔热物质上涌的高点是正确的。渤海凹陷及周边地区的高热流值(1.8—2.36)是有深部背景的。指出,地下热物质上涌及由于地壳不均匀性引起的温度场的水平梯度与华北地区的地震活动有密切的关系。

This paper presents the tentative knowledge on the basis of the studies of U Au ore deposits and mantle xenoliths. (1) the magma differentiated hydrothermal solutions are unreasonable; (2) the alkaline metasomatism is the key to understanding of the mantle and crust metasomatism; (3) the detachment structure is the channel of the upwelling mantle fluids; (4) the phosphor(P) is the characteristic tracer component of mantle fluids; (5) the ocean anoxic events, El Nino and black shales have the common...

This paper presents the tentative knowledge on the basis of the studies of U Au ore deposits and mantle xenoliths. (1) the magma differentiated hydrothermal solutions are unreasonable; (2) the alkaline metasomatism is the key to understanding of the mantle and crust metasomatism; (3) the detachment structure is the channel of the upwelling mantle fluids; (4) the phosphor(P) is the characteristic tracer component of mantle fluids; (5) the ocean anoxic events, El Nino and black shales have the common causes (HACONS upwelling effects); (6) natural gases oil oil shales salts hot brines hydrothermal ore formation constructed oregenesis systems, which are the derivatives of HACONS. The asthenospheric bodies and low velosity zones can be considered as the new prognostic targets.

通过铀、金矿床及地幔岩捕虏体研究,初步得出以下认识:(1)在热液作用中岩浆分异热液是不存在的;(2)碱交代作用是整个地幔交代作用和地壳交代作用的基本运作机制,现已构成有几十条具体规律的理论系统;碱交代岩是地幔流体转变为热液的化石记录;(3)拆离断层构造体系是地幔流体上升到地壳后的活动通道;(4)磷(P)是地幔流体的特征性示踪成分;(5)大洋缺氧事件、生物种属灭绝、厄尔尼诺等有共同的地幔流体致因;(6)天然气-油-盐-金属成矿是统一的热液成矿作用。软流体是今后区域成矿预测的重要新依据。软流体的顶部发育有次级、再次级的局部上凸部,这是矿带、矿田群的重要成矿控制因素和找矿新标志。

This paper reviews the new achievement of mantle convection research. The evolution characters of the subducted slabs, the driving mechanism of the upwelling mantle plume and its impact on the shallow structure are discussed. And the influence of the upwelling mantle plume on the formation and filling pattern of the extending basins, taking the North Sea Basin and the Jiyang Depression as instances, are analyzed especially. It is concluded that the rhythmicity of basin evolution is attributed to...

This paper reviews the new achievement of mantle convection research. The evolution characters of the subducted slabs, the driving mechanism of the upwelling mantle plume and its impact on the shallow structure are discussed. And the influence of the upwelling mantle plume on the formation and filling pattern of the extending basins, taking the North Sea Basin and the Jiyang Depression as instances, are analyzed especially. It is concluded that the rhythmicity of basin evolution is attributed to the mantle convection.

回顾近十年来在地幔对流方面的最新研究进展,阐述了板块俯冲后在地幔中的演化特征,以及地幔上升流即地幔柱的驱动机制和地质效应。特别介绍了地幔柱对地壳表层拉张盆地形成和充填过程的影响。进一步探讨了地幔柱活动在济阳坳陷的地质表现及其引发的火山岩浆活动、碎屑充填特征。认为盆地演化的阶段性间接反映了地幔对流的阶段性。

 
<< 更多相关文摘    
图标索引 相关查询

 


 
CNKI小工具
在英文学术搜索中查有关the upwelling mantle的内容
在知识搜索中查有关the upwelling mantle的内容
在数字搜索中查有关the upwelling mantle的内容
在概念知识元中查有关the upwelling mantle的内容
在学术趋势中查有关the upwelling mantle的内容
 
 

CNKI主页设CNKI翻译助手为主页 | 收藏CNKI翻译助手 | 广告服务 | 英文学术搜索
版权图标  2008 CNKI-中国知网
京ICP证040431号 互联网出版许可证 新出网证(京)字008号
北京市公安局海淀分局 备案号:110 1081725
版权图标 2008中国知网(cnki) 中国学术期刊(光盘版)电子杂志社