岩浆水的英文

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"岩浆水"怎么读用"岩浆水"造句

英文翻译手机版

juvenile water
magmatic water
magmaticwater
water， magmatic

"岩浆"英文翻译 magma; rock-magma
"水"英文翻译 water
"岩浆水沉积物" 英文翻译 : magmatic sediment
"岩浆水汽喷发" 英文翻译 : hydromagmatic eruption
"岩浆水沈积物" 英文翻译 : magmatic sediment
"浆水" 英文翻译 : starch solution; mixed starch; seriflux
"岩浆" 英文翻译 : [地] magma; rock-magma
"胞浆水" 英文翻译 : amniotic fluid
"浆水泵" 英文翻译 : proportioning pump; pull-out type pump; pulp water pump; pulwater pump
"浆液；浆水" 英文翻译 : seriflux
"泥浆水" 英文翻译 : earthy water; muddy water; slime water; slimewater
"糖浆水" 英文翻译 : molasses water
"芽浆水" 英文翻译 : mash liquor
"纸浆水泵；浆水泵" 英文翻译 : pulwater pump
"浆水平衡" 英文翻译 : water and fiber balance
"泥浆水力学" 英文翻译 : mud hydraulics
"泥浆水龙带" 英文翻译 : flexible mud hose
"泥浆水泥侵" 英文翻译 : cement cut
"石灰浆水" 英文翻译 : milk of lime
"血浆水解物" 英文翻译 : hydrolysate plasma
"纸浆水泵" 英文翻译 : pulwater pump
"油井灌浆水泥" 英文翻译 : oil-well grouting cement
"治疗血浆水平" 英文翻译 : therapeutic plasma level
"干岩浆" 英文翻译 : dry magma
"母岩浆" 英文翻译 : mother magma; parent magma; parental magma

例句与用法

From the study of hydrogen - oxygen isotope in enclosure liquid , some water conies from magma , others come from atmosphere precipitation
包裹体水的氢氧同位素研究表明成矿流体中既有岩浆水，又有大量大气降水加入。
The h and o isotope of water in fluid - inclusion at the beishan deposit indicates that the ore - forming fluid originated from magmatic water and partly from volcanic vapor
氢氧同位素研究证明，北山矿床成矿流体来源于原生岩浆水，有部分火山蒸气加入。
Hydrogen and oxygen isotopic composition of the fluid inclusion in quartz indicates that the water in ore - forming fluid was derived meanly from mixture water of meteoric and magmatic
石英流体包裹体氢氧同位素组成表明，成矿流体中的水主要来源于大气降水和岩浆水的混合。
The analyses of oxygen and hydrogen isotope indicate that the hydrothermal fluid is dominated by magmatic water with input of a lot of meteoric and underground water in the later stage
包裹体的氧、氢同位素特征表明，成矿热液虽以岩浆水为主，但在晚期有较多天水及地下水的混入。
The mineralization temperature is in a range of 90 ~ 300 , and the mineralization fluid is a combination of slightly acidic - slightly alkalic precipitations , seawater and magmatic water
其成矿温度在90 ~ 300之间，成矿流体为低盐度的弱酸性弱碱性大气降水、海水和岩浆水的混合溶液。
It is a result which oxidizes the environment that science measures the candy jade , and after hetian jade take shape , by incomplete for yu magma water along and hetian jade ore body crack permeate , it is oxidize there aren t iron not inferior not to make
经科学检测糖玉是氧化环境的产物，系和阗玉形成后，由残馀岩浆水沿和阗玉矿体裂隙渗透，使氧化亚铁转化三氧化二铁的结果糖皮即为氧化铁染的结果。
It belongs to nacl - h2o - co2 system . the ore - forming element assemblage is as - sb - cu - ni - u with high contents of as and sb . the stable isotope data show the metallogenic fluid comes from the mixture of magmatic water with meteoric water and stratum water
流体中成矿元素组合为as - sb - cu - ni - u ，总体上具较高的sb ， as含量；稳定同位素特征表明成矿溶液主要来自岩浆水与大气降水、沉积盆地地层水的混合。
Alkali basite , which came from upper mantle or lower crust , invaded through those structure , which not only bring cu et al mineralizing elements , but also the most important is that thermal energy . it cycled the formation water ( yinmin fonnation and luoxue formation ) , and form alkali - rich , middle - high temperature and salinity fluid mixed with alkali - rich magmatic water . there were high rate of percolation and well voidage in the contact zone between yinmin purple stratum and yinmin rubblerocks , which is in favor of the transposition and mineralization of minerogenetic fluids
因此，总结东川稀矿山式铜矿成矿模式为沉积( fe 、 cu ) ?热液叠加( cu )改造：晋宁-澄江期，小江深大断裂发生走滑运动，在东川矿区造成右行旋扭及其派生构造，形成“ z ”字形落因破碎带，同时来自深源(下地壳或上地幔)碱基性岩浆侵入，不仅带来了大量cu等成矿物质，更重要的是提供了热源，促使地层水(落雪组白云岩和因民组紫色层)循环，与富碱( na和k )岩浆水混合，形成富碱中高温高盐度流体。