- 更多网络例句与五角十二面体相关的网络例句 [注：此内容来源于网络，仅供参考]
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Gastaldi and co-workers have observed two types of contrasts in Al-Pd-Mn IQCs: black-white double-lobe and loop-shaped, by using X-ray topography, and the facetted dodecahedral pores by phase-sensitive radiography.
Gastaldi领导的小组在结合利用X射线形貌术以及相位敏感成像术研究Al-Pd-Mn二十面体准晶单晶中的缺陷时发现两种衬度，其中已知黑白双瓣衬度是由于准晶中的五角十二面体空洞引起，而对于环形衬度则除了知道退火行为不同于位错从而不太可能是位错圈外，基本上对其缺陷的几何及性质不甚了解。
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However, when occurring in Mesozoic remelted granite, pyrite is featured mainly by high gold content in pentagonal dodecahedron and in its complex; low content in cubic pyrite; Au/Ag ratio between 1-2; both N and P types of pyrite present in most deposits and P type only in a few deposits.
产于中生代重熔花岗岩中时，黄铁矿以五角十二面体居多，五角十二面体及其聚形含金较高，立方体含金性较差；Au/Ag比值在1-2之间，As的含量较高(＞600×10〓)；Co、Ni的含量则较低，一般为10n×10〓；热电性以既有P型又有N型的P、N混合型为特征，少数金矿床表现为单一的P型。
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The results show that the fine-grained hypidiomorphic pyrite, with a crystal form of pentagonal dodecahedron, contains more Au than others. Since the areas yield pyrite with relatively lower contents of main components S and Fe, while a greater gross content of trace elements, such as Cu, Pb, Zn, Au, Ag, are closely associated with gold deposits, the authors propose that a middle-scale gold deposit might be found in Zhaojiapuzi area; and there is a remote possibility to find a large gold deposit in Shengjingao area, wih a prospect of finding a concomitant gold deposit.gold deposits;mineralogical.
结果表明以五角十二面体晶形为特征的半自形细粒状黄铁矿含金性较高；黄铁矿主成份S、Fe含量相对低，而黄铁矿中Cu、Pb、Zn、Au、Ag等微量元素总量相对高的黄铁矿分布区城与金矿化关系密切；提出赵家堡子地区具备找到一处中型以上金矿的前景，而在生金皋地区找到大型金矿床的可能性很小，但有望找到伴生金矿床。
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Located in the prospecting lines Nos.47 and 37-33 on the middle 270m section, the mineral typomorphic characteristics are as follows: pyrite possesses the combination of octahedron with pyritohedron, pyritohedron with octahedron, etc It appearsas hole-centre and mix center conduction, if being electron-centre conduction, the absolute magnitudes of thermoelectromotive force and thermoelectromotive coefficient of pyrite are bigger relatively; pyrite contains Cu; the relative absorbency in quartz D(subscript H2O0.9403, D(subscript CO2)0.1961, D(subscript CO2)/D(subscript H2O)0.2591 in prospecting lines 37-33 is smaller than average D(subscript H2O1.3267, D(subscript CO2)0.3090, D(subscript CO2)/D(subscript H2O)0.338 2 in the deposit.
江西茅排金矿区270m中段47勘探线及37~33勘探线的矿物标型特征为：黄铁矿形态见有八面体和五角十二面体，五角十二面体和八面体等聚形；出现空穴心型导电和混合型导电黄铁矿，若为电子心型导电黄铁矿，其热电动势和热电系数的绝对值相对较大；黄铁矿成分中检测出Cu；石英相对吸光度（37~33勘探线）D(下标 H2O)0.9403，D(下标 CO2)0.1961，D(下标 CO2)/D(下标 H2O)0.2591，略低于矿区研究样品的平均值D(下标 H2O1.3267，D(下标 CO2)0.3090，D(下标 CO2)/D(下标 H2O)0.3382。
- 更多网络解释与五角十二面体相关的网络解释 [注：此内容来源于网络，仅供参考]
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pentagonal dodecahedron：五角十二面体
常温、常压下,气体分子在水中的溶解度很低,但在特定温压值(通常是高压、低温的环境)中(见下图),水分子之间会重新键结、排列成晶笼化合物(clathrate),形成五角十二面体(pentagonal dodecahedron)和五角十二面六角二面体(tetrakaidecahedron)两种结构(见下方晶笼结构图),
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pentagonal icositetrahedron：五角三八面体
五角半面像 pentagonal hemihedry | 五角三八面体 pentagonal icositetrahedron | 五角十二面体 pentagonal-dodecahedron
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pentagonal icositetrahedron：五角偏方三八面体
五角半面像 pentagonal hemihedry | 五角偏方三八面体 pentagonal icositetrahedron | 五角十二面体 pentagonal-dodecahedron
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pyritohedral：五角十二面体的
pyrite 黄铁矿 | pyritohedral 五角十二面体的 | pyritohedron 五角十二面体
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pyritohedral class：五角十二面体晶族
"胶黄铁矿","Pyritogelite" | "五角十二面体晶族","pyritohedral class" | "五角十二面体半面像","pyritohedral hemihedral class"
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pyritohedral hemihedral class：五角十二面体半面像
"五角十二面体晶族","pyritohedral class" | "五角十二面体半面像","pyritohedral hemihedral class" | "五角十二面体","pyritohedron"
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pyritohedron：五角十二面体
五角三八面体|pentagonal icositetrahedron, pentagonal trioctahedron | 五角十二面体|pyritohedron | 五台阶段|Wutaian stage
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negative pyritohedron：负五角十二面体
"negative pole","负极、阴极" | "negative pyritohedron","负五角十二面体" | "negative rain","负电荷雨"
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positive pyritohedron：正五角十二面体
(地壳)上升运动 positive movement | 正五角十二面体 positive pyritohedron | 正电荷雨 positive rain
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pyritoid：五角十二面体
"五角十二面体","pyritohedron" | "五角十二面体","pyritoid" | "黄铁矿形","Pyritoidal form"