Journal of the Mineralogical Society of Japan最新文献_第3页

北海道札幌市小別沢鉱山産のテルル鉱物(Poughite, Frohbergite, Melonite)について关于北海道札幌市小别泽矿山所产的碲矿物(Poughite, Frohbergite, Melonite)

Journal of the Mineralogical Society of Japan Pub Date : 1991-07-31 DOI: 10.2465/GKK1952.20.89

博行井伊, 昭彦岡田

引用次数: 0

鉱物標本管理・検索システムの構築と運用--地質調査所地質標本館での実体験から矿物标本管理与检索系统的构建与运用——来自地质调查所地质标本馆的实际体验

Journal of the Mineralogical Society of Japan Pub Date : 1991-07-01 DOI: 10.2465/GKK1952.20.133

Y. Sakamaki, Chisayo Matsue

引用次数: 1

惑星科学における鉱物学の役割とその将来 (鉱物学からみた固体地球・惑星科学の展望 ) 矿物学在行星科学中的作用及其未来(从矿物学的角度展望固体地球和行星科学)

Journal of the Mineralogical Society of Japan Pub Date : 1990-07-01 DOI: 10.2465/GKK1952.19.283

土山明

引用次数: 0

分析電子顕微鏡による粘土鉱物の分析--装置メ-カ-の立場から (熱水変質作用と粘土鉱物の生成) 分析电子显微镜下的黏土矿物的分析——从设备的角度(热液变质作用和黏土矿物的生成)

Journal of the Mineralogical Society of Japan Pub Date : 1990-03-01 DOI: 10.2465/GKK1952.19.SPECIAL_131

柴富邦夫

引用次数: 0

Mechanism of smectite-to-illite conversion. 蒙脱石转化成伊利石的机理。

Journal of the Mineralogical Society of Japan Pub Date : 1990-03-01 DOI: 10.2465/GKK1952.19.SPECIAL_53

A. Inoue

引用次数: 1

岐阜県恵那郡蛭川村田原の日本新産鉱物,ヒンガン石,ヘランド石,ウォッジナ石岐阜县惠那郡蛭川村田原的日本新产矿物，蛭石，蛭石，蛭石

Journal of the Mineralogical Society of Japan Pub Date : 1987-05-20 DOI: 10.2465/GKK1952.18.17

律郎宮脇, 泉中井, 弘三長島, 鑑吉岡本, 敏雄磯部

{"title":"岐阜県恵那郡蛭川村田原の日本新産鉱物,ヒンガン石,ヘランド石,ウォッジナ石","authors":"律郎宮脇, 泉中井, 弘三長島, 鑑吉岡本, 敏雄磯部","doi":"10.2465/GKK1952.18.17","DOIUrl":"https://doi.org/10.2465/GKK1952.18.17","url":null,"abstract":"Hingganite, hellandite and wodginite occur in druse type pegmatite in quarries at Tahara, Hirukawa-mura, Ena-gun, Gifu prefecture, Japan. Two kinds of hingganite, (Y1.22Ca0.26…)Σ1.91Fe2+0.09Be2.08Si2.08O8.09(OH)1.91 and (Ce0.54Y0.51Nd0.31…)Σ2.08Fe2+0.41Be1.96Si1.96O8.87(OH)1.13, were found as colorless (hingganite-(Y)) to light brown (hingganite-(Ce)) euhedral crystals associated with quartz, feldspar, mica, cassiterite, stokesite, flourite, chlorite, sphene, and an unknown mineral chemically related to hingganite. Hellandite, (Ca5.75Y3.70Nd0.24Dy0.21…)Σ10.65 (AI1.45Mn0.25Ti0.21Fe0.11) (OH)4[Si8B8O40.22(OH)3.78] occurs as an aggregate of colorless transparent crystals covering surface of hingganite. The associated minerals of hellandite are quartz, flourite, chlorite and zeolite group minerals. Wodginite, Mn3.84 (Sn1.53 Ti1.11Fe3+0.60W0.31Ta0.27Zr0.18) (Ta7.99Nb0.01)O32 occurs as a black prismatic crystal on feldsper, associated with quartz, mica, topaz, beryl, flourite. The chemical compositions and X-ray crystallographic data of these minerals are given and are compared and discussed with data previously reported. Lattice parameters: Hingganite-(Ce), monoclinic, a=9.996(10), b=7.705 (7), c=4.792(4) A, β=90.06(4)°; Hellandite, monoclinic, a=18.91(2), b=4.684(6), c=10.30(6) A, β=111.7(1)°; Wodginite, monoclinic, a=9.513(9), b=11.456(12), c=5.108(4) A, β=91.09(9)°.","PeriodicalId":242743,"journal":{"name":"Journal of the Mineralogical Society of Japan","volume":"23 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"1987-05-20","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"127853707","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

引用次数: 1

続成・熱水変質作用におけるイライト/スメクタイト及び3入面体型緑泥石/スメクタイト混合層鉱物の生成と変化续成和热液变质作用中异石/湿石石和三面体绿泥石/湿石石混合层矿物的生成和变化

Journal of the Mineralogical Society of Japan Pub Date : 1986-03-20 DOI: 10.2465/GKK1952.17.SPECIAL_75

厚行井上

{"title":"続成・熱水変質作用におけるイライト/スメクタイト及び3入面体型緑泥石/スメクタイト混合層鉱物の生成と変化","authors":"厚行井上","doi":"10.2465/GKK1952.17.SPECIAL_75","DOIUrl":"https://doi.org/10.2465/GKK1952.17.SPECIAL_75","url":null,"abstract":"Conversion processes of illite/smectite and chlorite/smectite interstratified minerals during burial diagenesis and hydrothermal alteration are characterized from the standpoints of their structural and chemical changes. The decrease in expandability of illite/smectite takes place nearly continuously from 100 % to 0%, although the diagenetic and hydrothermal conversion processes are characterized by slightly different conversion trends. On the other hand, that of chlorite/smectite takes place discontinuously in both environments, with steps at about 100-80 %. 50-40%, and 15-0%. With such structural changes, illite/smectite gradually decreases the tetrahedral Si and octahedral Mg and increases the tetrahedral and octahedral Al and interlayer K. The chemical changes for chlorite/smectite take place apparently continuously from saponite to chlorite following that the tetrahedral Al and octahedral Fe increase and the tetrahedral Si and interlayer Ca decrease. In terms of chemical composition, a 1:1 regularly interstratified mineral, rectorate, has distinctive characteristics from those of common illite/smectite questioned here, as well as its distinctive structure. In chlorite/smectite, it is noticeable that there is a discordance between the discontinuous decrease in expandability and the continuous change in chemical composition during the aggrading conversion.","PeriodicalId":242743,"journal":{"name":"Journal of the Mineralogical Society of Japan","volume":"37 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"1986-03-20","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"131403293","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

引用次数: 0

ハロイサイトの熱的特性,特に示差走査熱量分析(D.S.C.)による脱水エネルギーについて关于褐藻细胞的热特性，特别是示差扫描热量分析(d.s.c.)的脱水能量

Journal of the Mineralogical Society of Japan Pub Date : 1986-03-20 DOI: 10.2465/GKK1952.17.SPECIAL_163

秀雄湊, 治彦難波

{"title":"ハロイサイトの熱的特性,特に示差走査熱量分析(D.S.C.)による脱水エネルギーについて","authors":"秀雄湊, 治彦難波","doi":"10.2465/GKK1952.17.SPECIAL_163","DOIUrl":"https://doi.org/10.2465/GKK1952.17.SPECIAL_163","url":null,"abstract":"Halloysite (10 A), one species of kaolin minerals, changes to metahalloysite by heating at 30-120°C with the loss of water and also changes to metakaolin by heating at 350-550°C with the loss of water or hydroxyl ion. Halloysite shows two different shapes under the electron microscope, such as tubular and spherical, and is formed by two different geological conditions, by hydrothermal reaction and weathering reaction. The differences of thermal properties on halloysites of different shapes and different modes of occurrence are investigated by means of thermogravimetry and differential scanning calorimetry. And dehydration energies of the first and the second stages are measured as cal/gram for the following five halloysite specimens. Two tubular materials from Tawara, Naegi, Gifu Prefecture and Mikuni, Kato-gun, Hyogo are tested, the former one is formed by hydrothermal reaction and the latter one is formed by weathering reaction. The other two materials of spherical shape from Ookuchi mine, Kagoshima Prefecture and from ma mine, Nagano Prefecture are also tested, the former one is formed by hydrothermal reaction and the latter one is formed by weathering reaction. The purified four materials are measured by the same methods, and the first stage dehydration energies are nearly the same value for the four specimens and the values are nearly equal to that of the latent heat of water evaporation. The values of the second stage dehydration energy for the four materials are different and the materials formed by hydrothermal reaction have higher value than that of the materials formed by weathering reaction in the both crystal forms. And the spherical materials have higher values than of tubular shape ones. These differences caused by their crystallinity, shapes of crystal, modes of occurrences, etc. Halloysite material with high grade of crystallinity occurred from the Dragon mine, Utah, U.S.A.. It is also tested by the same methods for the dehydration energies in the first stage and the second stage; both the values are higher than that of the four materials above mentioned.","PeriodicalId":242743,"journal":{"name":"Journal of the Mineralogical Society of Japan","volume":"43 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"1986-03-20","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"120904897","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

引用次数: 0

多摩丘陵中部,上総層群に見られる粘土鉱物の検討その1 多摩丘陵中部，上总层群中发现的黏土矿物的研究之一

Journal of the Mineralogical Society of Japan Pub Date : 1986-03-20 DOI: 10.2465/GKK1952.17.SPECIAL_35

吉宏坂本

引用次数: 0

スメクタイトの熱分析--特に100℃付近の吸熱ピ-クについて (粘土鉱物の生成と変化の機構) 粘土矿物的热分析——特别是100℃附近的吸热皮(粘土矿物的生成和变化机制)

Journal of the Mineralogical Society of Japan Pub Date : 1986-03-01 DOI: 10.2465/GKK1952.17.SPECIAL_147

坂本尚史

引用次数: 0