{"title":"岐阜县惠那郡蛭川村田原的日本新产矿物，蛭石，蛭石，蛭石","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":null,"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":0.0000,"publicationDate":"1987-05-20","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"1","resultStr":"{\"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\":null,\"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\":0.0000,\"publicationDate\":\"1987-05-20\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"1\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Journal of the Mineralogical Society of Japan\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.2465/GKK1952.18.17\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Journal of the Mineralogical Society of Japan","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.2465/GKK1952.18.17","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
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)°.
求助内容：
应助结果提醒方式：
京公网安备 11010802042870号
