绿帘石的英文

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"绿帘石"怎么读用"绿帘石"造句

英文翻译手机版

acanthicone
acanthiconite
acanticone
acanticonite
achmatite
akanthikon
akanticone
allochite
bragationite
delphinite
epidosyte
epidote-tremolite schist
fouqueite
pistacite

"绿"英文翻译 green
"石"英文翻译 dan,a unit of dry measure fo ...
"暗绿帘石" 英文翻译 : arendalite; arendite
"多色绿帘石" 英文翻译 : taimowite
"铬绿帘石" 英文翻译 : chrome eqidote; chrome pistazite; chromepidote; cr epidote; tawmawite
"含铈绿帘石" 英文翻译 : cerium epidote
"黄绿帘石" 英文翻译 : delphinite
"绿帘褐帘石" 英文翻译 : epidote orthite
"绿帘石的" 英文翻译 : epidotic
"绿帘石化" 英文翻译 : epidotization
"绿帘石属" 英文翻译 : epidote group
"绿帘石岩" 英文翻译 : epidosite; epidotite
"镁绿帘石" 英文翻译 : picroepidote
"锰绿帘石" 英文翻译 : manganepidote
"铅绿帘石" 英文翻译 : hancockite
"铁绿帘石" 英文翻译 : ferriepidote
"透绿帘石" 英文翻译 : oisanite
"黄绿色绿帘石" 英文翻译 : thallite
"绿帘石闪石岩相" 英文翻译 : epidote amphibolite facies
"绿帘石化作用" 英文翻译 : epidotization
"形成绿帘石的" 英文翻译 : epidotized
"原矿变绿帘石" 英文翻译 : palaeoepidote
"变绿帘石原矿物" 英文翻译 : palaeoepidote
"绿帘石化玄武岩" 英文翻译 : creoline
"绿帘石角闪岩相" 英文翻译 : epidote amphibolite facies; epidote-amphibolite facies

例句与用法

Epidote may be quite conspicuous .
绿帘石有时相当显著。
The ore ' s mineral component is simple , and its main association of minerals are leucocratic sphalerite - galenite ? iopsite ( epidot , chlorite ) . leucoratic sphalerite and diopsite are the guide minerals in the ore
主要矿物组合为浅色闪锌矿-方铅矿-透辉石(绿帘石、绿泥石) ，其中浅色闪锌矿和透辉石为该类矿石的标型矿物。
Under the hydrodynamitic condition in the outshelf heavy minerals are enriched to a certain extent . they are of horablede - epidote assemblage and contain some authigene ( pyrite and glauconite ) . the content of stable mineral is small and mineral maturity index ( trzg / hp ) is low
在外陆架水动力的作用下，重矿物有一定富集，重矿物以角闪石?绿帘石矿物组合为特征，含有一定量自生矿物(黄铁矿和海绿石) ，稳定矿物少，矿物成熟度低。
The microscopical observation proves that the main types of granitoid rocks are granodiorite and quartz monzodiorite , and the enclave is mainly monzodiorite . the rock - forming minerals are mainly k - feldspar , plagioclase , amphiboie , biotite , quartz , magnetite , titanite , apatite , epidote , etc . the zonation of the feldspars is very popular . the dark - colored minerals , such as biotite and titanite , have been highly oxidized
通过对本区花岗岩类样品进行显微观察研究，知其主要的岩石类型为花岗闪长岩、石英二长闪长岩，其中的岩石包体主要为二长闪长岩，其造岩矿物为钾长石、斜长石、角闪石、黑云母、石英、磁铁矿、榍石、磷灰石和绿帘石等，长石中环带现象比较常见，黑云母、榍石等暗色矿物颜色较深，表明其氧化程度较高。
There are lots of primary structures , such as bed interfaces , lagerklufts and diagonal joints , in the emeishan volcanic , which dislocated to be dislocation interfaces later . especially in those primary structures that were filled with the epidote - quartz vein , the dislocation interfaces are more aptter to grew
错动带主要是利用玄武岩中原生层面、层节理和斜节理等原生构造错动变形而成，尤其是当原生构造中充填有热液型绿帘石?石英脉时，错动变形更易于发生。