the upper crust中文是什么意思

• 面包的表皮

• "upper crust"中文翻译    〔美俚〕上层阶级；头，脑袋。
• "upper crust" 中文翻译 :    〔美俚〕上层阶级；头，脑袋。
• "upper-crust" 中文翻译 :    n.,adj. 1.(馅饼、面包等的)上外皮(的)。 2.〔美口〕上层阶级(的)。 3.〔俚语〕头(的)。
• "crust" 中文翻译 :    n. 1.面包皮 (opp. crumb)；干面包片；生活口粮，糊口之资。 2.外皮，壳；〔美国〕雪壳；【地质学；地理学】地壳；【动物；动物学】甲壳；【医学】痂；(酒等的)浮渣；水垢。 3.(事物的)皮相，外表，表面。 4.〔美俚〕老面皮，厚颜无耻，没礼貌；(人的)脑壳。 crust movement 地壳移动。 earn one's crust 挣钱糊口。 have a crust 〔美俚〕脸皮太厚；太大胆，太鲁莽，太冒失。 the upper crust 〔古、俚〕上层社会。 vt.,vi. 用外皮覆盖；结成硬皮；生痂儿。 The snow has crusted over. 雪在地上结成冰壳。
• "upper" 中文翻译 :    adj. 1.(更)上面的，上方的，上部的；较高的；上级的；(议会)上院的；(衣服)穿在外面的。 2.上流的；高原地带的；内地的。 3.【地质学；地理学】地表层的；〔常 U-〕后期的。 the upper seats [circle] (戏院的)楼座，花楼。 the upper lip 上唇。 get [have] the upper hand of 胜过，占上风[优势]。 n. 1.〔常 pl.〕鞋面皮，鞋帮；〔pl.〕布绑腿；〔口语〕(车船卧铺的)上铺。 2.〔美俚〕兴奋剂，刺激性药物〔尤指安非他命〕。 (down) on one's uppers 鞋底完全磨平；非常贫穷。
• "aging crust" 中文翻译 :    老化的地壳
• "airytype crust" 中文翻译 :    艾里型地壳
• "algal crust" 中文翻译 :    藻壳; 藻皮
• "and a crust of bread" 中文翻译 :    和一片硬面包
• "attenuation of crust" 中文翻译 :    地壳减薄
• "basaltic crust" 中文翻译 :    玄武岩壳
• "blood crust" 中文翻译 :    血痂
• "botryoidal crust" 中文翻译 :    葡萄状皮壳
• "bread crust" 中文翻译 :    面包皮
• "breakable crust" 中文翻译 :    易碎雪层
• "buckling of crust" 中文翻译 :    地壳弯曲
• "buffy crust" 中文翻译 :    白细胞层; 血沉棕黄层
• "calc crust" 中文翻译 :    钙质壳
• "calcareous crust" 中文翻译 :    代钙质地表层；石灰结皮；石灰结壳; 钙积层; 钙质壳; 石灰性结壳
• "cobalt crust" 中文翻译 :    八水合砷酸钴
• "continental crust" 中文翻译 :    大陆板块; 大陆地壳；陆壳; 大陆型地壳; 陆壳
• "coral crust" 中文翻译 :    珊瑚薄盖层
• "cork crust" 中文翻译 :    木栓壳
• "crack a crust" 中文翻译 :    生活得还不错, 收入尚堪自给
• "cratonic crust" 中文翻译 :    克拉通地壳

• Depths of these hypocenters concentrate at about 12km deep in the upper crust .
  这些震源深度集中在地壳上部约12公里处。
• The deformations at the surface of the crust after rainfalls have close relations to the occurrence of shallow shocks in the upper crust .
  雨后地壳表面的形变与地壳上部发生的浅源地震密切相关。
• These studies , therefore , suggest that the songsugou peridotite is not a tectonic massif of the upper mantle but a ultramafic magmatic rock body crystallized in deep crust and tectonically emplaced in the upper crust
  从而证明了松树沟橄榄岩体并不是上地幔岩石的残片，而是由岩浆在深部地壳环境下结晶而成并以固态构造侵位于地壳的上部。
• 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。
• The surface loading of the mountains and the associated root of thickened crust produce horizontal deviatoric tension in the strong upper crust . in contrast , the deep , dense lithospheric root and its associated downflexing of the surface produce horizontal compressive deviatoric stress in the strong near - surface layer . the actual state of stress in the strong layer of the upper crust is the combined effect of these two opposite stress systems together with bending and other local and regional stresses such as due to ridge push
  模拟结果表明：由于均衡机制，造山带下部的低密度山根促使地壳隆升、造山，山根是地壳刚性层中张性构造应力的主要力源；与此相反，冷的高密度岩石圈向软流圈插入、拆离、下沉，从而形成岩石圈根，它引起挤压造山和岩石圈地幔物质的重新调整，也是地壳刚性层中挤压性构造应力的主要力源。
• Based on the study on ree distribution characteristics of sinian low grade metamorphic rocks of the basement and cover volcanics , the author makes a discussion on the material source and the genesis of xiangshan volcanics , and suggests that xiangshan volcanics came mostly from the remelting of the upper crust , and the genesis should be attributed to the category of remelted granites
  摘要本文通过对相山火山盆地基底震旦系浅变质岩、盖层火山岩稀土元素分布特徵的研究，探讨相山火山岩的物质来源及岩石成因，认为相山火山岩主要是上部地壳重熔的产物，其岩石成因应属于重熔型花岗岩的?畴。
• Studies on geology of the deposits and geochemistry of trace elements , rees , isotopes , ore - forming fluids show that the ore - forming materials came from varied sources . ore - forming materials of the tianbaoshan deposit was chiefly derived from different sedimentary rocks of the upper crust and orogen , while those of the daliangzi deposit mainly from the sinian dengying formation . meteoric waters were the major source of the ore - forming solution
  矿床地质特征以及常微量元素、稀土元素、同位素、成矿流体等地球化学特征的研究表明，矿床成矿物质是多来源的，天宝山矿床成矿物质主要来自上部地壳和造山带各种沉积岩，大梁子矿床成矿物质主要来自震旦系灯影组地层；两个矿床成矿溶液主要来自大气降水；硫大部分来源于同时期的海相沉积地层(震旦系灯影组)中被细菌还原的海水硫酸盐。
• 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。

• the upper crust in Hindi