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Miyahisaite, a new mineral 宫石,一种新矿物
Q4 Earth and Planetary Sciences Pub Date : 2015-01-01 DOI: 10.2465/GKK.141215B
D. Nishio–Hamane
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引用次数: 0
Development of the three-dimensional visualization system for crystal, volumetric and morphology data and its application to mineralogical sciences 晶体、体积和形态数据三维可视化系统的开发及其在矿物学中的应用
Q4 Earth and Planetary Sciences Pub Date : 2015-01-01 DOI: 10.2465/gkk.141216
K. Momma
Threedimensional visualization system VESTA and maximumentropy method (MEM) analyses program Dysnomia have been developed for mineralogical and crystallographic studies. VESTA seamlessly visualizes multiple numbers of crystal, volumetric and morphology data in a same graphic window. It can calculate and output a variety of crystallographic information. Dysnomia is much faster than its predecessor PRIMA, and has several new features including a brandnew LBFGS algorithm and a new type of constraints. Dysnomia is virtually integrated with a pattern ˆtting system RIETANFP for the MEMbased pattern ˆtting. These programs have been widely used in thousands of researches not limited to mineralogy but also in a variety of areas including chemistry, materials science, bioscience, electronic state calculations and so on.
开发了三维三维可视化系统VESTA和最大熵法(MEM)分析程序Dysnomia,用于矿物学和晶体学研究。VESTA在同一图形窗口中无缝地可视化多个晶体,体积和形态数据。它可以计算和输出各种晶体学信息。Dysnomia比它的前身PRIMA快得多,并且有几个新功能,包括一个全新的新的LBFGS算法和一种新的约束类型。Dysnomia实际上集成了一个模式排版系统RIETANFP用于基于MEM的模式排版。这些程序已广泛应用于数千项研究,不仅限于矿物学,而且还应用于化学、材料科学、生物科学、电子态计算等各个领域。
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引用次数: 0
Chemistry of chromian spinels in serpentinites from the North Shimanto belt, western Shikoku, Japan 日本西部四国岛东带北部蛇纹岩中铬尖晶石的化学特征
Q4 Earth and Planetary Sciences Pub Date : 2015-01-01 DOI: 10.2465/GKK.140708
Y. Ichiyama
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引用次数: 0
Global lithium resources —Overview of various deposit types and ore genesis inferred from lithium isotopes— 全球锂资源-从锂同位素推断的各种矿床类型和矿床成因概述-
Q4 Earth and Planetary Sciences Pub Date : 2015-01-01 DOI: 10.2465/GKK.150206
D. Araoka
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引用次数: 0
宮城県北部,石越安山岩の地質・岩石学的特徴とマグマプロセス;宮城県北部,石越安山岩の地質・岩石学的特徴とマグマプロセス;Geology, petrology and magma process of Ishikoshi Andesite in northern Miyagi Prefecture, NE Japan 宫城县北部,石越安山岩的地质、岩石学特征和岩浆过程;宫城县北部,石越安山岩的地质、岩石学特征和岩浆过程;Geology, petrology和magma process of Ishikoshi Andesite in northern Miyagi Prefecture, NE Japan
Q4 Earth and Planetary Sciences Pub Date : 2015-01-01 DOI: 10.2465/gkk.140811
Kei Sato, Akira Ishiwatari
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引用次数: 0
Oxidation state of Fe within olivine phenocryst in Kami-Kometsuka scoria, Kami-Kometsuka, Aso, Kumamoto Prefecture, Japan: effect of high temperature oxidation on the scoria 日本熊本县阿索Kami-Kometsuka矿渣中橄榄石斑晶铁的氧化态:高温氧化对矿渣的影响
Q4 Earth and Planetary Sciences Pub Date : 2015-01-01 DOI: 10.2465/GKK.150816
T. Ejima
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引用次数: 2
Spatial variation of Sr-Nd-Hf isotopic compositions in from Cretaceous to Paleogene granitoids from Northeastern Japan Arc 日本岛弧东北部白垩系至古近系花岗岩Sr-Nd-Hf同位素组成的空间变异
Q4 Earth and Planetary Sciences Pub Date : 2015-01-01 DOI: 10.2465/GKK.130830
Y. Hirahara, R. Senda, Toshiro Takahashi, Nobutaka Tsuchiya, Shin‐ichi Kagashima, Takeyoshi Yoshida, Q. Chang, T. Miyazaki, S. V. Bogdan, J. Kimura
(平成 25 年 8 月 30 日受付,平成 26 年 12 月 31 日受理,平成 27 年 3 月 20 日早期公開,担当編集委員亀井淳志特集号ゲスト編集 委員) (独)海洋研究開発機構地球内部ダイナミクス領域,〒2370061 横須賀市夏島町 215 現所属千葉工業大学工学部,〒2750016 千葉県習志野市津田沼 2171 新潟大学大学院自然科学研究科,〒9502181 新潟市西区五十嵐二の町 8050 † 岩手大学教育学部,〒0208550 盛岡市上田 3188 †† 山形大学理学部,〒9908560 山形市小白川町一丁目 412  東北大学理学部,〒9808578 仙台市青葉区荒巻字青葉 63 Institute For Research on Earth Evolution, Japan Agency for MarineEarth Science And Technology, Yokosuka 2370061, Japan Email: yuka8685@wine.ocn.ne.jp Present address: Departmentof Physics, Chiba Institute of Technology, Tsudanuma, Chiba 2750016, Japan Faculty of Science, Niigata University, 8050, Ikarashi 2nocho, Nishiku, Niigata 9502181, Japan † Faculty of Education, Iwate University, Ueda, Morioka 0208550, Japan †† Faculty of Science, Yamagata University, 412 KojirakawaMachi 1Chome, Yamagata 9908560, Japan  Faculty of Science, Tohoku University, Aoba, Sendai 9808578, Japan 岩石鉱物科学 44, 91111, 2015
(平成 25 年 8 月 30 日受付,平成 26 年 12 月 31 日受理,平成 27 年 3 月 20 日早期公開,担当編集委員亀井淳志特集号ゲスト編集 委員) (独)海洋研究開発機構地球内部ダイナミクス領域,〒2370061 横須賀市夏島町 215 現所属千葉工業大学工学部,〒2750016 千葉県習志野市津田沼 2171 新潟大学大学院自然科学研究科,〒9502181 新潟市西区五十嵐二の町 8050 † 岩手大学教育学部,〒0208550 盛岡市上田 3188 †† 山形大学理学部,〒9908560 山形市小白川町一丁目 412  東北大学理学部,〒9808578 仙台市青葉区荒巻字青葉 63 Institute For Research on Earth Evolution, Japan Agency for MarineEarth Science And Technology, Yokosuka 2370061, Japan Email: yuka8685@wine.ocn.ne.jp Present address: Departmentof Physics, Chiba Institute of Technology, Tsudanuma, Chiba 2750016, Japan Faculty of Science, Niigata University, 8050, Ikarashi 2nocho, Nishiku, Niigata 9502181, Japan † Faculty of Education, Iwate University, Ueda, Morioka 0208550, Japan †† Faculty of Science, Yamagata University, 412 KojirakawaMachi 1Chome, Yamagata 9908560, Japan  Faculty of Science, Tohoku University, Aoba, Sendai 9808578, Japan 岩石鉱物科学 44, 91111, 2015
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引用次数: 4
第一原理計算による理論高圧鉱物物性学の開拓;第一原理計算による理論高圧鉱物物性学の開拓;Creation of the ab initio theoretical high-pressure mineral physics 基于第一原理计算的理论高压矿物性学的开拓;基于第一原理计算的理论高压矿物性学的开拓;创造of the ab initio theoretical high-pressure mineral physics
Q4 Earth and Planetary Sciences Pub Date : 2015-01-01 DOI: 10.2465/GKK.150104
T. Tsuchiya
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引用次数: 0
化学風化の速度論:流紋岩風化の野外調査,室内実験および理論解析 化学风化速度论:流纹岩风化的野外调查,室内实验及理论分析
Q4 Earth and Planetary Sciences Pub Date : 2015-01-01 DOI: 10.2465/GKK.141214
正人 横山
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引用次数: 0
鉱物科学から断層摩擦のメカニズム解明に挑む;鉱物科学から断層摩擦のメカニズム解明に挑む;A challenge for understanding the friction of faults from mineral science 从矿物科学入手阐明断层摩擦的原理;从矿物科学入手阐明断层摩擦的原理;理解挑战the friction of faults from mineral science
Q4 Earth and Planetary Sciences Pub Date : 2015-01-01 DOI: 10.2465/GKK.141215A
Hiroshi Sakuma
Maximum friction coe‹cients of common minerals can be characterized by empirical Byerlee's rule, however, some important faultforming minerals such as mica and clay minerals have ultimately low friction coe‹cient. The layered structure and high a‹nity to water should be related to the low friction coe‹cient. We have investigated the interlayer bonding energy, adsorption energy of water molecules, and physical properties of adsorbed water by using molecular simulations, surface xray scattering, and surface forces measurements. These results were used for interpreting the weak friction coe‹cients of layered minerals.
常见矿物的最大摩擦系数可以用经验Byerlee法则来表征,而一些重要的断层形成矿物如云母和粘土矿物的最终摩擦系数较低。层状结构和对水的高亲和性应与低摩擦系数有关。我们利用分子模拟、表面x射线散射和表面力测量研究了层间键能、水分子的吸附能和吸附水的物理性质。这些结果用于解释层状矿物的弱摩擦成分。
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引用次数: 0
期刊
Japanese Magazine of Mineralogical and Petrological Sciences
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