oceanic crust中文是什么意思

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用"oceanic crust"造句"oceanic crust"怎么读"oceanic crust" in a sentence

中文翻译手机版

(洋壳)大洋地壳
海康地壳
海洋板块
海洋地壳
洋底壳
洋壳

"oceanic"中文翻译 adj. 1.大洋的，大海的；大洋广的，(生活)在大洋中 ...
"crust"中文翻译 n. 1.面包皮 (opp. crumb)；干面包片；生 ...
"average oceanic crust structure" 中文翻译 : 平均洋壳结构
"igneous oceanic crust" 中文翻译 : 火成岩洋壳
"intervening oceanic crust" 中文翻译 : 插入的洋壳
"large slices of oceanic crust" 中文翻译 : 洋壳的大块解体
"magnetic stripes of the oceanic crust" 中文翻译 : 大洋地壳磁条带
"normal oceanic crust" 中文翻译 : 标准洋壳
"oceanic block of crust" 中文翻译 : 大洋地壳块
"oceanic-continental crust boundary" 中文翻译 : 大洋地壳与大陆地壳边界
"pristine oceanic crust" 中文翻译 : 古洋壳
"quasi-oceanic crust" 中文翻译 : 类洋壳
"subducted oceanic crust" 中文翻译 : 俯冲洋壳
"oceanic" 中文翻译 : adj. 1.大洋的，大海的；大洋广的，(生活)在大洋中的；大洋一样的，广阔无边的。 2.〔O-〕大洋洲的。
"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。
"oceanic-oceanic convergence" 中文翻译 : 海洋-海洋型聚敛作用
"oceanic-oceanic magma" 中文翻译 : 海洋-海洋型岩浆
"itt oceanic" 中文翻译 : 国际电话电报大洋公司
"itt-oceanic" 中文翻译 : 国际电话电报大洋公司
"oceanic absorption" 中文翻译 : 海洋吸收
"oceanic abstracts" 中文翻译 : 海洋学文摘数据库
"oceanic acoustics" 中文翻译 : 海洋声学
"oceanic airlines" 中文翻译 : 海洋航空
"oceanic ak" 中文翻译 : 欧欣尼克
"oceanic anticyclone" 中文翻译 : 副热带高压; 洋面反气旋

例句与用法

Owing to the difficulty of sampling beneath the deep oceans, the composition of the oceanic crust is not known with complete certainty .
由于在深海底下取样困难，海洋地壳的组成就不完全确知。
Shrimp dating of carboniferous jinshajiang ophiolite in western yunnan and sichuan : geochronological constraints on the evolution of the paleo - tethys oceanic crust
古特提斯洋壳演化的同位素年代学制约
Zhang j . x . and meng f , c . 2006 . lawsonite - bearing eclogites in the north qilian and north altyn tagh : evidence for cold subduction of oceanic crust . chinese sciernce bulletin , 51 ( 10 ) : 1238 - 1244
张建新,孟繁聪, 2006 .北祁连和北阿尔金含硬柱石榴辉岩：冷洋壳俯冲作用的证据.科学通报， 51 ( 14 ) (即刊)
The authors put forward that daba - xiugugabu ophiolite belt originated from an ancient oceanic crust fragment of india continental northern marginal ocean basin , that was approximately synchronous with the formation and evolution period of the neo - tethys ocean
笔者提出该区蛇绿岩来源于印度大陆北缘洋盆的洋壳碎片，这个陆缘洋盆与新特提斯洋主体的形成和演化准同步。
Among different opinions , the most popular one is that the temporal and spatial distribution and evolution of the gangdise plutonic - volcanic belt are controlled by the northward subduction of the yarlung zangbo oceanic crust and the southward subduction of the bangong - nujiang oceanic crust
在众多的观点中较权威的观点，是冈底斯岩浆带的时空分布与演化受控于雅鲁藏布江洋壳和班公湖-怒江洋壳分别向北向南俯冲。
Combining the isotope geochronological results with the fieldwork observations , we could draw some conclusions as follows : the kunlun - bayan har terranes experienced the subduction of oceanic crust and collision somewhat earlier than the bayan har - qiangtang terranes , with only a very short interval in between and even the collisions overlapped partially in time
_ 2 ： 227 - 218ma ，巴颜喀拉和羌塘之间洋壳俯冲，以金沙江岩带iag型岩浆侵位为标志。 _ 3 ： 217 - 212ma ，造山后期岩浆侵位。
In the northern part , the oceanic crust occurring between the bayan har and kunlun terranes started subduction from south to north at about 243 ma , and did not stop until the development of post - orogenic pog - type granite in the bayan har terrane at 220 ma , thus illustrating the orogeny in the form of subduction and collision kept active for over 20 ma
以pog型花岗岩在巴颜喀拉地体内大量生成、在阿尼玛卿岩带中较多出现、在昆仑岩带利金沙江岩带少量出现为标志。期： 160 - 140ma ，断裂系活动；金沙江、东昆仑剪切作用发生；部分岩体动力变质变形。
Based on the regional geologic survey on the scale of 1 / 250 000 , coupled with geological , geochemical and geophysical investigations in some key regions , this dissertation summarized the tectonomagmatic evolution and mineralization of the mid - gangdise area . with respect to tectonic evolution , the gangdise belt has experienced a multi - stage evolutional history since mesozoic , including oceanic crust subduction , arc - continent collision , intracontinental subduction and collision , and strike - slip and block uplift
论文以新一轮1 ： 25万区域地质调查为基础，在对关键区段重点解剖的基础上，结合地球物理、岩石化学、地球化学、沉积作用、变质作用、构造演化和成矿作用的研究成果，对冈底斯中段的构造岩浆演化与成矿作了较系统的科学总结。