混杂岩的英文

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"混杂岩"怎么读用"混杂岩"造句

英文翻译手机版

block clay
contaminated rocks
contaminatedrock
hybrid rocks
melange

"混杂"英文翻译 mix; mingle; confounding; so ...
"岩"英文翻译 rock
"钙质混杂岩" 英文翻译 : calcimixtite
"构造混杂岩" 英文翻译 : tectonic melange
"巨屑混杂岩" 英文翻译 : chaos
"前缘混杂岩" 英文翻译 : front melange
"蛇绿混杂岩" 英文翻译 : ophiolitic melange; ophioliticmelange
"方解辉长混杂岩" 英文翻译 : hortite
"自生碎屑混杂岩" 英文翻译 : autoclastic melange
"杂岩" 英文翻译 : complex rock; diamictite; rock complex
"甘肃红石山地区蛇绿混杂岩地质特征" 英文翻译 : geological characteristics of ophiolite migmatitic complex of hongshishan region gansu
"混杂" 英文翻译 : (混合搀杂) mix; mingle; confounding; sophistication 鱼龙混杂 good and bad people get mixed up; 游客混杂 visitors of all kinds; 它与其他很多东西混杂在一起了。 it was confused among many objects
"斑杂岩" 英文翻译 : taxites
"杂岩，硬岩" 英文翻译 : graywacke
"杂岩盐" 英文翻译 : halo-sylvite
"高混杂" 英文翻译 : upperr hybrid
"合混杂" 英文翻译 : interweave
"混合,混杂" 英文翻译 : commingle
"混杂岸" 英文翻译 : hybrid rock
"混杂的" 英文翻译 : farraginous; hybrid; jumbly; magpie; miscellaneous; mixed; promiscuous
"混杂度" 英文翻译 : impurity
"混杂货" 英文翻译 : heterogenous cargo; mixed cargo
"混杂料" 英文翻译 : adulterant
"混杂名" 英文翻译 : nomen confusum
"混杂物" 英文翻译 : farrago; hodgepodge; impurity; mishmash; olio

例句与用法

Study of mesozoic palaeotectonic stress field in the volcamic rock area of huzhong , the northern part of dahinganling volcanic zone
青海省阿尼玛卿带布青山蛇绿混杂岩的地球化学性质及形成环境
Dege - xiangcheng metallogenic belt are formed in stretching vocalnic island arc , and the ore - foming process is related with vocalnic - sedimenting tightly
金矿床大多赋存于板块结合带内的蛇绿混杂岩带中。
There exists a series of meso - neoproterozoic tectonic melanges and ophiolitic melanges in jianping - fuxin - tieling area of northern liaoning province
摘要辽宁北部建平阜新铁岭地区，存在一套中新元古代构造混杂岩系、蛇绿混杂岩。
The basic to ultra - basic rocks are distributed along suture zones , whereas the intermediate to acidic intrusives occur mainly to the south and north of the arsuo tectonic melange zone and the angren ophiolitic melange zone
基性-超基性岩沿结合带分布，而中酸性侵入岩主要分布在阿索蛇绿混杂岩和昂仁蛇绿混杂岩的南北两侧。
The geochemical characteristics of gabbros from the jinshajiang ophiolitic melange indicate that they were derived from a mantle source different from that of volcanic rocks , which may be a product in the ocean rift in the earlier stage
东竹林蛇绿混杂岩中辉长岩地球化学特征表明，它与火山岩不同源，可能是洋盆裂谷初期的产物。
Based on the 1 / 250000 mapping work of yutian and bolike sheets , an early paleozoic ophiolite melange has been found in western kunlun mountain and named as qimanyuter ophiolite melange ( qom ) . this ophiolite melange is exposed along the north flank of kunlun mountains , from south of pulu - liushui village yutan county to south of nuer of ciler county
在本论文工作所依托的1 ： 250000于田和伯力克两幅区域地质调查工作中，发现了一条早古生代的蛇绿混杂岩带，我们将其命名为其曼于特蛇绿混杂岩带。
Thus , they might be derived from a back - arc basin with an archipelagic system in paleo - tethys , instead of a large ocean basin . the isotopic geochemistry shows that the jinshajiang ophiolitic melange has higher e nd ( t ) values ( + 7 . 42 - + 5 . 44 ) , suggesting that it may be derived from a lree depleted mantle source without significant contamination by the continental crust , but affected slightly by a fluid from a subducted ocean crust
同位素地球化学研究表明，金沙江蛇绿混杂岩具有较高的_ ( nd ) ( t )值( + 7 . 42 + 5 . 44 )暗示蛇绿岩来源于lree长期较亏损的地幔源，演化过程中没有受到陆源物质的明显混染，而主要受到少量俯冲洋壳析出流体的影响。
Qimanyuter ophiolite melange crops out 1 - 3 km in width and extends ew - nee about 50 km , parallels to the kunlun mountains . qimanyuter ophiolite melange is composed mainly of serpentinite ( metapyrolite ) , peridotite , bedded gabbro , grbbro , diabase sheet and pillow - like and massif basalt as well . associated sedimentary rocks with this ophiolite melange include silicalite , dark gray silicalite and thin - bedded limestone
该混杂岩带所包含的主要岩性单位包括：蛇纹岩(变辉橄岩) 、橄榄辉石岩、层状辉长岩、辉长岩、辉绿岩席、枕状、块状、杏仁状玄武岩，与之共生的沉积岩为紫红色硅质岩、深灰色硅质岩、薄层灰岩等。
During this evolution , seven second - order tectonic units were formed ; from north to south are the mingqianri cretaceous residual sea basin , the arsuo tectonic melange zone , the taricuo - wenbu yenshan magmatic arc belt , the cuoqin - bangduo late paleozoic composite back - arc basin , the jiangrang - geerdi faulted uplift , the gangdise - chazi himalayan magmatic arc belt , and the xigaze - anba fore - arc basin . these units comprise important parts of a poly - arc - basin system and exhibit evolutional features of mesozoic to cenozoic arc - basin systems . mosaic pattern of these tectonic units delineates the lithosphere coupling processes of the gangdise tectonic belt under mechanisms such as back - arc basin attenuation and arc - continent collision
自中新生代以来，冈底斯构造带经历了洋壳俯冲、弧陆碰撞、陆内俯冲-碰撞、走滑和块段隆升的多阶段构造演化历程，形成了由北向南七个二级构造单元，即岷千日白垩纪残余海盆、阿索构造混杂岩带、它日错?文部燕山期岩浆弧带、措勤?帮多晚古生代复合弧后盆地、江让?格尔耿断隆、冈底斯?查孜喜马拉雅期岩浆弧带、日喀则?安巴弧前盆地。
Based on the geological , stratigraphic and geochemical characteristics of the ophiolitic melange , island - arc and rift volcanic rocks from the jinshajiang zone , an archipelagic tectonic model with multi - rift and multi - subduction is proposed to explain the evolution of jinshajiang paleo - tethys . the ophiolitic melanges of the jinshajiang zone are mainly outcropped at baimangxueshan , tongduo , gongka , dongzhulin and jiyidu in the deqin county . the geochemistry of major and trace elements of the jinshajiang ophiolite shows its geochemical characteristics are similar to those of the more and island - arc volcanic rocks , but different from those of the typical n - mopjb
金沙江蛇绿混杂岩主要分布在德钦县的白茫雪山、通多、共卡、东竹林和吉义独地区，主量和微量元素地球化学特征研究表明，金沙江蛇绿岩不具有典型n - morb的地球化学特征，而具有介于morb和岛弧之间的地球化学特征，暗示它并非形成于宽阔的大洋环境，不是古特提斯在滇西北地区的主缝合带，可能是古特提斯多岛洋体系中的一个弧后盆地。