enstatite中文是什么意思

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中文翻譯
造句

n.
【地質(zhì)學(xué)；地理學(xué)】頑火輝石(巖) (＝protobastite)。

chondrite of enstatite 頑火輝石球粒隕石
enstatite achondrite 頑火輝石無球粒隕石
enstatite basalt 頑火玄武巖
enstatite chondrite 頑火輝石球粒隕石
enstatite diabase 頑火輝綠巖; 頑火輝石輝綠巖
enstatite diopside 頑透輝石
enstatite diopsidite 頑火透輝石巖
enstatite dunite 頑火純橄欖巖
enstatite hornblendite 頑火角閃石巖
enstatite limburgite 頑火?；x橄巖
enstatite norite 頑火蘇長巖
enstatite peridotite 頑火橄欖巖
enstatite plagiaplite 頑火斜長細(xì)晶巖
enstatite porphyrite 頑火玢巖
enstatine 頑輝石
enstar corp 恩斯塔公司
enstadite 頑輝石
enst bretagne 電信學(xué)院
ensslin 恩斯林

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例句與用法

The relationship between shock wave velocity and particle velocity of no - porous enstatite can be expressed as : d = 3 . 771 + 1 . 516u where the unit of velocity is km / s
可以認(rèn)為，從p phugongiot數(shù)據(jù)看，在50 160gpa范圍內(nèi)，頑火輝石的高壓相是穩(wěn)定的。
( 3 ) by using the new method put out in ( 2 ) , hugoniot data of no - porous samples of enstatite ( mg0 . 92 , fe0 . 08 ) sio3 which initial density is 3 . 273g / m3 , were reduced and the modified hugoniot data shows very small dispersivity
（ 3 ）用（ 2 ）中提出的新方法，對前人和本文的頑火輝石hugongiot實(shí)驗(yàn)數(shù)據(jù)進(jìn)行了初始孔隙度修正。結(jié)果顯示，不同研究者所得的hugongiot數(shù)據(jù)的分散性大大減小。
So it is impossible for enstatite to decompose to oxides between 50 to 140gpa . ( 5 ) the bulk modulus k0s and its first derivative of pressure k0s " were calculated from the experimental hugoniot data , by using eularian limit strain theory
3 ）根據(jù)本文頑火輝石hugoniot實(shí)驗(yàn)數(shù)據(jù)（結(jié)合前人的實(shí)驗(yàn)數(shù)據(jù)l用歐拉有限應(yīng)變理論計(jì)算得到的頑火輝石零壓炸彈性模量及其對壓力的一階導(dǎo)數(shù)為： k叮一266gpa ， k ；，二4
The linear relationship between shock wave velocity d and particle velocity u of our samples were obtained : d = 3 . 701 + 1 . 527u there the unit of relocity is km / s . no phase transition shows for enstatite with perovskite structure according to the experimental linear d - u line up to 110gpa
實(shí)驗(yàn)結(jié)果表明，在80 115gpa壓力范圍內(nèi)本文所用頑火輝石的沖擊波速度d與粒子速度u可用線性關(guān)系： d = 3 . 247 + 1 . 626u來描述。
Considering that no phase transition of enstatite with perovslite structure were found during these static high pressure experiments , the consistence of the bulk modulus also supports that the high pressure phase of perovskite structure of enstatite is stability between 50 - 140gpa
考慮到靜高壓下的數(shù)據(jù)是在實(shí)驗(yàn)中未發(fā)現(xiàn)頑火輝石高壓相有相變的情況下得到的。因此，動高壓與靜高壓實(shí)驗(yàn)數(shù)據(jù)的一致性支持了在80 ? 140gpa壓力內(nèi)預(yù)火輝石的高壓相保持穩(wěn)定的觀點(diǎn)。
( 4 ) the hugoniot of the mixture of mgo ( mw ) and sio2 ( st ) were calculated by the additire principle of hugoniot for mixture , and compared with the experimental hugoniot of enstatite . the results shows that there exists large difference between both d - u relationship and p - n curve for the two hugoniot
516u （ 4 ）用混合物hugongiot線的疊加性原理計(jì)算了mgo （ mw ）和引。（ st ）混合體系的hugongiot線，經(jīng)過與頑火輝石實(shí)驗(yàn)hugongiot數(shù)據(jù)對比，無論是從心關(guān)系還是從一產(chǎn)關(guān)系上看兩者均有較大差距。
The main work and achierement are as following : ( 1 ) by using shock impedance matching technique and electric probe method , 5 shots of impact experiments were conducted to measure the hugoniot equation of state for enstatite ( mg0 . 92 , fe0 . 08 ) sio3 with the average initial density 3 . 05g / m3 from shock pressure 50 gpa to 115gpa , using two stage light gas gun
本文研究取得的認(rèn)識主要有以下幾點(diǎn)： ( 1 )用阻抗匹配法和電探針技術(shù)在80 115gpa壓力范圍內(nèi)對平均初始密度為3 . 05g / cm ~ 3的頑火輝石樣品進(jìn)行了5發(fā)hugoniot狀態(tài)實(shí)驗(yàn)測量。
Shock wave compression technique has play an important role in the understanding of the material composition thermodynamic state and physical properties of the earth ' s ulterior . in this article , the stabling of high - pressure phase of one of the main candidate materials of the earth ' s lower mantle ? enstatite ( mg0 . 92 , fe0 . 08 ) sio3 were investigated through the experimented measurement of hugoniot equation of state , and together with thermodynamic calculation and analysis
本學(xué)位論文以沖擊壓縮技術(shù)為手段，從測量其hugoniot物態(tài)方程入手，結(jié)合高壓物理和熱力學(xué)理論分析，較深入地研究了下地幔中的一種主要候選組分頑火輝石( mg _ ( 0 . 92 ) ， fe _ ( 0 . 08 ) ) sio _ 3在與下地幔大致相當(dāng)?shù)臏囟葔毫l件下的相態(tài)-鈣鈦礦型結(jié)構(gòu)的相穩(wěn)定性。

百科解釋

Enstatite is the magnesium endmember of the pyroxene silicate mineral series enstatite (MgSiO3) - ferrosilite (FeSiO3). The magnesium rich members of the solid solution series are common rock-forming minerals found in igneous and metamorphic rocks.

詳細(xì)百科解釋

其他語種釋義

enstatiteとは意味：{名} : 頑火輝石｛がんかきせき｝

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