上地壳的英文

• supracrust
• upper crust

• "上"英文翻译    upper; up; upward
• "地壳"英文翻译    the earth's crust
• "上地壳的" 英文翻译 :    supracrustal
• "上地壳建造" 英文翻译 :    supracrustal formation
• "上地壳侵蚀" 英文翻译 :    supracrustal erosion
• "上地" 英文翻译 :    earth; jochi; kamichi; uechi; uwachi
• "地壳" 英文翻译 :    [地质学] (the earth's) crust; shell◇地壳板块 crustal plate; 地壳变形 diastrophe; 地壳变动 diastrophism; 地壳波导 waveguide in earth crust; 地壳断裂 crustal fault; 地壳构造 earth crust structure; 地壳形变 crustal deformation; 地壳应力 crustal stress; 地壳运动 diastrophism; crustal movement; 地壳运动期 orocratic period
• "上地里" 英文翻译 :    go to field
• "上地利" 英文翻译 :    upper austria
• "上地幔" 英文翻译 :    earth upper mantle; peridotite shell; upper mantle
• "天上地" 英文翻译 :    celestially
• "无上地" 英文翻译 :    supremely
• "向上地" 英文翻译 :    antrorsely; skywards; upstream; upwards
• "至上地" 英文翻译 :    consummately
• "轴上地" 英文翻译 :    epaxially
• "地壳的" 英文翻译 :    crustal
• "地壳氦" 英文翻译 :    crust helium
• "地壳省" 英文翻译 :    crustal province
• "下地壳" 英文翻译 :    lower crust
• "原地壳" 英文翻译 :    protocrust
• "本质上地，实质上地" 英文翻译 :    c.in essence
• "本质上地" 英文翻译 :    c.in essence
• "表面上地" 英文翻译 :    seemingly
• "财政上地" 英文翻译 :    financially
• "传统上地" 英文翻译 :    traditionarily

• ( 3 ) the mineral source was provided by both lower crust , upper mantle and upper crust , obviously from crust - mantle mixing
  ( 3 )矿田中的成矿物质的不仅来自于下地壳和上地幔，而且还来自于上地壳，具有壳幔混合特征。
• The plumbum isotope of ores conform the mixture model of three components , the plumbum of earth ' s mantle , the plumbum of upper ea rth ' s crust and the plumbum of strata in the aketishikan gold deposit
  阿克提什坎金矿床矿石铅同位素符合三元混合模型，三端元为地幔铅、上地壳铅及地层铅。
• The round columnar joints show that the dyke swarms are in upper crust brittle tectonic setting , and the western shandong block is brittle extensional in the mesoproterozoic time
  岩墙发育圆柱状节理表明岩墙侵位时地块已经处于上地壳脆性构造环境,中元古代鲁西地区是一个脆性伸展的大地构造环境。
• The plumbum of ores belongs to the orogenic belt plumbu m , essentially is the mixture plumbum of earth ' s mantle and crust . the pl umbum originates from the orogenic belt and the metallization has relationship with the orogeny
  矿石铅既具有地幔铅的特征，又具有上地壳铅的特征，并且具有造山带铅的特点，成矿作用与造山作用关系密切，铅来源于造山带物质，本质上是壳幔混合铅。
• The characters of velocity ' s distribution within the mid - layer of the middle crust resemble that of the upper crust ' s bottom layer , and the velocity strongly disturbed . the prominent higher velocity anomalies exist below the linbi uplift and the hu - su uplift within this layer
  中地壳的中间层速度分的基本特征类似上地壳底部，横向均匀性显著；中地壳下部速横向不均匀性明显，在灵壁隆起和湖苏隆起的下部有显著的高速异常。
• During the yanshanian phrase , the area is in the condition of contractional background , with multi - staged tectonic reversion . 5 . through studying the origin of volcanic rocks and the characteristics of magma evolution , it concludes that there exist 3 originated areas of magma - from mantle , crust , and mantle - crust exchange . the basic magma of nandaling volcanic rocks of early jurassic is derived from upper mantle ; the magma of tiaojishan volcanic rocks of mid jurassic is formed in the contractional tectonic setting , and derived from the transition zone of crust and mantle interaction ; the acid magma of l
  5 、通过岩石化学、微量元素、稀土元素的研究，探讨了不同级别节律的火山岩成因、岩浆演化等特征，认为本区燕山期火山岩有三个岩浆源区，即地幔源、地壳源和壳幔混源，早侏罗世的南大岭旋回的基性岩浆，起源于上地幔；中侏罗世髫髻山旋回火山岩是在相对挤压环境中，岩浆起源于壳幔过渡带；晚侏罗世无负eu异常的酸性岩浆来源于下地壳的古老结晶基底的局部熔融，有负eu异常的酸性岩浆来源于上地壳的局部熔融；早白垩世火山岩基性岩浆起源于上地幔，中性岩浆起源于下地壳底部的壳幔过渡带。
• It shows that the resolution of the crust interface ' s shape on this four profiles is very good , nevertheless that of the velocity structure is relatively poor . the crust and upper mantle ' s fine configuration on the hq - 13 profile is obtained by our tomography , which reveals some important structure and dynamic features of this region : the velocity structure of the crust consists of three layers , the upper crust , the middle crust and the lower crust . however it also can be divided into six lateral blocks , each of them " s velocity is always higher or lower than that of its neighboring blocks
  本文第五章利用有限差分反演和射线反演的方法获得了符离集?奉贤地震测深剖面( hq - 13线)精细的地壳上地幔结构剖面，揭示出下扬子地区一些重要的结构和动力学特征：地壳速度结构在纵向上大致可分上地壳、中地壳和下地壳三部分，横向上可划分为6个块体，各块体的p波速度沿测线方向呈现高速?低速?高速的组合。
• Through the study of characteristic of macroelement , microelement , rare - earth element , oxyhydrogen isotope , sulfur isotope , lead isotope , fluid inclusion etc , a conclusion can be drawn that metallogenic substance comes from the upper mantle with mixing of some substance from the upper crust latter . it is likely to have the same source with the surrounding rock
  通过对矿床的常量元素、微量元素、稀土元素、流体包裹体特征、氢氧同位素、硫同位素、铅同位素等特征的研究，认为成矿物质主要来源于上地幔，与周围岩石存在着同源的可能性，后期有一定的上地壳物质混入，成矿作用有三期，分别与区内的花岗岩、二长花岗岩脉、云煌岩脉有关。

• 上地壳的法语：croûte supérieure
• 上地壳的俄语：внешняя оболочка
• 上地壳的阿拉伯语：القشرة الأرضية العليا;