- 更多网络例句与钠柱石相关的网络例句 [注：此内容来源于网络，仅供参考]
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For giving an explaintion of strong transmogrification but feebleness metamorphism of and their corresponding relation of the Triassic stratum in Songpan-Ganzi area and opening out the temperature and stress condition, this paper summarized study production of predecessors, and put forward 5 conclusions about Songpan-Ganzi area Triassic main lithology(slate, sandrock,and blastopsammitic) through field geological investigation , actual measurement section plane study and combining indoor slice identification , electron probing and fluid enclosure testing analysis:1.Field outcrop strongly transmogrification, and often developed same cleavages(S1) erection or approximately erection 'B'fold and symmetry similituded fold. 2.The metamorphosed mineral combination is simple, and the typical metamorphosed mineral combination is Al+Chl+Ser+Cc+Q, etc. The metamorphosed mineral develops mainly along the cleavages of the territorial cleavages faces(S1), bearing territorial dynamic metamorphism character and belonging to the lawsonite-albite-chlorite face of slightly metamorphism. 3.Territorial metamorphism P-T change focus on T:180～200oC, P:1～2kbar
为了对松潘-甘孜地区三叠系强变形浅变质的特征及变质与变形的对应关系作出解释，揭示变质与变形的温-压条件，本论文总结前人研究成果，通过野外地质调查和实测剖面研究，结合室内薄片鉴定、电子探针和流体包裹体测试分析，对松潘-甘孜地区三叠系主体岩性(板岩、砂板岩、变质砂岩及千枚岩)的变质作用得出5 个认识结论：1、整个松潘-甘孜地区经受了自北向南的强大挤压；2、变质矿物组合简单，除雏晶黑云母外，典型的变质矿物组合为Al+Chl+Ser+Cc+Q等，变质矿物主要沿区域性劈理面(S1)的劈理域发育，具有区域动力变质作用特征，属于低级变质作用中的硬柱石-钠长石-绿泥石相；3、区域变质作用P-T 变化集中在T：180～200oC，P：1～2kbar
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The sole gem marialite deposit in China is located at the western foot of Mount Muztagh,Akto County, Xinjiang, which is tectonically belongs to the Central Famirs fold belt.
中国已知的宝石级钠柱石矿床仅有一处，位于新疆阿克陶县苏巴什达坂北其依达克附近。
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The large tantalum niobium tungsten ore pertains to the fine-grained granite deposit of albite muscovite. The useful minerals mainly consist of wolframite and scheelite, and a small number of tantalum niobite, fine spar, tantalum aeschynite, beryl, and bismuth, etc.
该大型钽铌钨矿为细粒钠长石化白云母花岗岩矿床，主要有用矿物为黑钨矿、白钨矿及少量的钽铌铁矿、细晶石、钽易解石、绿柱石和辉铋矿等。
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The primary beryl crystals were crystallized early from the pegmatitic magma in association with rock forming minerals such as quartz, muscovite, albite and spodumene.
原生绿柱石形成于早期岩浆阶段，与造岩矿物石英、白云母、钠长石、锂辉石共生。
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On the basis of comprehensive discipline research, the rocks subfacies and microfacies of hydrothermal rocks facies have been initially studied and the their characteristic have been come to conclusions frist time.
在多学科综合研究基础上，首次系统提出研究并总结了热水沉积岩相的亚相及微相特征，亚相包括有：钠长岩-似碧玉岩亚相、硅质白云岩→硅质岩亚相、碱性钠长石质-碳酸质岩亚相、铁镁碳酸盐岩亚相、重晶石岩亚相、黑云母方柱石岩/黑云母岩亚相及铁绿泥石岩亚相。
- 更多网络解释与钠柱石相关的网络解释 [注：此内容来源于网络，仅供参考]
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dipsas plicatus：佛像珍珠
dipyre 针柱石钙钠柱石 同 dipyrite | dipsas plicatus 佛像珍珠 | dirigem 德莱宝石
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scapolite：柱石
方柱石(scapolite)是钠钙铝硅酸盐,并含有cl、f等阴离子,化学分子式为(na,ca)4(al(al,si)si2o8],(cl,f,oh,co3,so4)方柱石族矿物是以钠柱石和钙柱石为端元的类质同象系列的中间矿物.
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wernerite：钙钠柱石
Werner filtering 沃纳滤波 | wernerite 钙钠柱石 | werneritite 方柱石岩
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wernerite：方柱石;柱石
"Wernerian theory","韦氏学说" | "wernerite","方柱石;柱石" | "weslienite","锑钠钙石"
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berylloid：绿柱石晶状的
beryllocene | 二茂铍 | berylloid | 绿柱石晶状的 | beryllonite | 磷(酸)钠铍石
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Beryllonite 1：磷(酸)钠铍石 1
Beryl 1.577 绿柱石 1.577 | Beryllonite 1.553 磷(酸)钠铍石 1.553 | Chrome Green 2.4 铝铬绿 2.4
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dipyre：针柱石,钙钠柱石
双锥体,双角锥 dipyramid | 针柱石,钙钠柱石 dipyre | 针柱石,钙钠柱石 dipyrite
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marialite：钠柱石 亦称
margarita margaritifera,Linne 林纳贝 | marialite 钠柱石 亦称meionite | mari-diamond 马利钻石
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marialite：钠柱石
marginatus 有边缘的 | marialite 钠柱石 | marine algae 海洋藻类
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marialite：钠柱石 同
meerschaum 海泡石 | meionite 钠柱石 同 marialite | melange 混合品