mantle ['mæntl]

mantle的基本解释

n.

斗篷, 罩子, 覆罩之物

vt.

罩住, 覆盖

• Clouds mantled the moon.
• 云把月亮遮住。

• Snow mantled the trees.
• 雪覆盖了树木。

vi.

覆盖, 脸红

• The champagne mantled in the glass.
• 玻璃杯里的香槟酒面上泛起一层泡沫。

• The girl's face mantled in joy.
• 那姑娘高兴得脸上泛起红晕。

mantle的同义词

n. robe · cloak · coat · cover · wrap

mantle所属的单词分类

Furniture / 家具 [143]

window shades  ·  tea cart  ·  sleeper sofa  ·  office chair  ·  lounge chair  ·  lift chair  ·  kitchen island  ·  gateleg table  ·  garden bench  ·  Game table

Housing & Dwelling / 房屋与居住 [290]

yaodong  ·  tudor  ·  threshhold  ·  terraced house  ·  storage shed  ·  row house  ·  light switch  ·  garage door opener  ·  garage door  ·  fuse box

与mantle相关的网络例句 [注：此内容来源于网络，仅供参考]

The relationship between mantle fluid and U ore-forming was studied preliminarily,according to the results,the author considered theΣCO_2 of mineralizer and heat source came from mantle,which is because upwelling mantle forced by crustal extention and deep-seated faulting produced melt blending with lower crust,during this process,mantle provided the heat and releaseΣCO_2 to crust through outgassing.U mainly came from mantle-curst fluid formed by mantle-curst melt blending and the wall rock during fluid uplift.H_2O mainly generated from mantle fluid and the wall rock during mantle fluid uplift,and partly from atmospheric water in the late period of ore-forming.

初步探讨了地幔流体与铀成矿作用的关系，认为矿化剂∑CO_2和热源来源于地幔，是地壳拉张和深大断裂活动导致部分熔融地幔上涌，与下地壳产生壳幔混熔作用，在混熔过程中提供热量和向地壳&去气&释放∑CO_2；U主要来源于壳幔混熔形成的壳幔混合流体和流体上升途经的围岩；H_2O主要来源于地幔流体、地幔流体上升途经的围岩，在成矿晚期有部分来源于大气降水。

Based on the settings and geological and geochemical characteristics of granitoids of different orogenic belts (exemplified by orogenic granitoids in Altay, East Kunlun, Yanshan in North China, Northeast China and Nanling in South China), the relationships between granitoids and continental crustal growth are discussed, and five modes of continental crustal growth in the continent of China are proposed;they are as follows:(1)the Altay mode of continental growth is that the material and heat of the Paleozoic convertive mantle formed on the background of the Paleo-Asian Ocean were input into the Paleozoic continent and mixed with the materials of the upper crust;(2) the East Kunlun mode is that the basement of the Proterozoic orogenic belt was reworked by the heat input and materials of the Paleozoic-early Mesozoic convective mantle formed on the background of TTG continental crust of the Proterozoic orogenic belt;(3) the Northeast China style is that the Phanerozoic continental crust was reworked by the heat input and materials from the convective mantle formed on the background of the Yanshanian Central Asian orogenic belt;(4) the Yanshan mode is that the Archean basement was reworked by the heat input and materials from the Yanshanian convective mantle;and (5) the Nanling mode is that in South China what was input by the Yanshanian convective mantle into the continent was mainly heat and subordinately materials and the crustal material recycle was the dominant mode for the continental growth (showing zero continental growth).

根据不同造山带花岗岩的形成背景，地质地球化学特征差异，以阿尔泰，东昆仑，华北燕山，东北和南岭造山带花岗岩为例讨论花岗岩与大陆地壳生长的关系，区分出中国大陆的5种大陆地壳生长方式：阿尔泰式是古亚洲洋背景上形成的古生代对流地幔物质，热输入和上地壳混合为主的方式；东昆仑式是元古代造山带TTG陆壳背景基础上古生代—早中生代对流地幔物质和热输入，改造元古宙造山带基底的方式；东北式是燕山期中亚造山带背景上对流地幔物质和热输入改造显生宙陆壳的生长方式；燕山式是燕山期对流地幔物质和热输入改造太古宙基底的方式；南岭式燕山期对流地幔输入大陆的是以热为主，物质为辅，大陆地壳生长是以陆壳物质再循环为主的生长方式。

The earth is a complicated system, and it has been continuously moving differentiating and evolving since it had been formed. Not only has the earth layering structure, but it has vertical movement of materials. The movement is prompted by the mechanism of force and heat of the centrifugal force to be formed by the rotation and revolution of the earth, and difference of temperature, pressure, density, viscosity and velocity in the between core and mantle, and radioactive heat, et al. The expressive means of the mechanism of force and heat are the precesses of mantle plume and mantle fluid. Not only are ore-materials of core and mantle carried directly into crust, but ore-materials of crust are activated and accumulated into proper location by the mantle fluid having the supercritical nature.

地球是一个复杂的系统，自形成以来，一直处于不停地运动、分异和演化过程；它不仅存在着圈层结构，而且伴随其自转和公转的离心力，以及核幔间的温度差、压力差、密度差、粘度差、速度差和放射性蜕变热等动热机制，同时存在着以地幔柱和地幔流体作用方式的物质垂向运动；这一过程，不仅直接向地壳带入核幔成矿物质，而且通过流体自身的超临界性质，将沿途活化已有初步富集的成矿物质转移至地壳适宜部位集中成矿。

与mantle相关的网络解释 [注：此内容来源于网络，仅供参考]

mantle：地幔

依据震波速度之不连续性,可将地球内部分成(由上而下):地壳(EarthCrust),地幔(Mantle)及地核(Core)三带. 此分带与上述分圈不同. 软流圈大致相当于上部地幔,中心圈大致相当于下部地幔及地核.

mantle：斗篷

她在1998年装置作品斗篷(mantle)给我重重的一击. 现在美国迈阿密艺术博物馆. 看看那女人身后的六万支鲜花!沉静的女人手中的线团,落地玻璃窗外洒进来的光亮!那种美惊心动魄又不动声色,震撼了十二岁的我,如今再看依旧是震撼再震撼.

mantle：外套膜

large opening,与适当大小的byssus结合,croceas可以牢固的附着在底层,特大的pedal外套膜(mantle)可以完全扩张和收缩(下面有介绍). 关于软体部分,croceas扩张外套膜(mantle),超出贝壳上部边缘,从上面看完全将贝壳遮住.

mantle：地函

依据震波速度之不连续性,可将地球内部分成(由上而下):地壳(EarthCrust),地函(Mantle)及地核(Core)三带. 地壳和地函之间的分界面被称为「莫霍界面」(Moho discontinuity)莫氏不连续面岩石圈(Lithosphere)下之软层圈为软流圈(Asthenosphere)属於上部地函(upper mantle)海洋的外壳通常比较薄,

mantle, cloak：斗篷

dust coat 风衣 | mantle, cloak 斗篷 | poncho 篷却(南美人的一种斗篷)