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The chemical analysis of ferroaxinite is SiO_2 42.40,Al_2O_3 18.30,Fe_2O_3 0.09,TiO_2 0.13,FeO 9.05,MgO 1.51,MnO 0.77,CaO 19.20,B_2O_3 6.37,H_2O^+ 1.33,H_2O^- 0.06,total 99.21% corresponding to ( Ca_\u003cl.94\u003eMn_\u003c0.06\u003e)_\u003c〓2.00\u003e (Fe^\u003c2+\u003e_\u003c0.71\u003eMg_\u003c0.21\u003eAl_\u003c0.04\u003eFe^\u003c3+\u003e_\u003c0.01\u003eTi_\u003c0.01\u003e )_\u003c〓0.98\u003eAl_\u003c2.00\u003eB_\u003cl.04\u003eSi_\u003c4.00\u003eO_\u003c16\u003eH_\u003c0.84\u003e on the basis of total O = 16. The empirical formula of datolite, derived from the chemical analysis, is very close to the ideal formula CaBSiO_5 (OH) with a slight H_2O excess. Idiomorphic forms of the minerals are exclusively found in voids in veins, although partially developed forms of ferroaxinite are common. Ferroaxinite is tabular with largerr(011) and b(010). Datolite idiomorphs are short prisms with m(110) and s(102) dominant. Associated minerals within and adjacent to veins are quartz, calcite, albite, adularia, chlorite, and bannisterite, together with pumpellyite. In veins ferroaxinite always preceeds datolite in the crystallisation sequence. This is similar to the relationship between manganaxinite and datolite in skarns from some pyrometasomatic ore deposits in Kyushu. 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Ferroaxinite and datolite from Mt. Nio, Shizuoka city, central Japan(MEMORIAL VOLUME TO THE LATE PROFESSOR TERUHIKO SAMESHIMA)
https://doi.org/10.14945/00000309
https://doi.org/10.14945/00000309a7822e03-766e-4a1d-8dec-5649f1e4fae9
名前 / ファイル | ライセンス | アクション |
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KJ00000102352.pdf (313.0 kB)
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Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||||
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公開日 | 2008-01-25 | |||||||
タイトル | ||||||||
言語 | en | |||||||
タイトル | Ferroaxinite and datolite from Mt. Nio, Shizuoka city, central Japan(MEMORIAL VOLUME TO THE LATE PROFESSOR TERUHIKO SAMESHIMA) | |||||||
言語 | ||||||||
言語 | eng | |||||||
キーワード | ||||||||
言語 | en | |||||||
主題Scheme | Other | |||||||
主題 | ferroaxinite | |||||||
キーワード | ||||||||
言語 | en | |||||||
主題Scheme | Other | |||||||
主題 | datolite | |||||||
キーワード | ||||||||
言語 | en | |||||||
主題Scheme | Other | |||||||
主題 | pumpellyite | |||||||
キーワード | ||||||||
言語 | en | |||||||
主題Scheme | Other | |||||||
主題 | Setogawa Group | |||||||
資源タイプ | ||||||||
資源タイプ識別子 | http://purl.org/coar/resource_type/c_6501 | |||||||
資源タイプ | departmental bulletin paper | |||||||
ID登録 | ||||||||
ID登録 | 10.14945/00000309 | |||||||
ID登録タイプ | JaLC | |||||||
著者 |
Sameshima, Teruhiko
× Sameshima, Teruhiko
WEKO
252
× Ono, Susumu |
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書誌情報 |
Geoscience reports of Shizuoka University 巻 20, p. 1-4, 発行日 1994-03 |
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出版者 | ||||||||
出版者 | Shizuoka University. Institute of Geosciences | |||||||
NDC | ||||||||
主題Scheme | NDC | |||||||
主題 | 458 | |||||||
抄録 | ||||||||
内容記述タイプ | Abstract | |||||||
内容記述 | Ferroaxinite and datolite occur in veins in a dolerite sheet cutting metabasite of the Setogawa Group. The chemical analysis of ferroaxinite is SiO_2 42.40,Al_2O_3 18.30,Fe_2O_3 0.09,TiO_2 0.13,FeO 9.05,MgO 1.51,MnO 0.77,CaO 19.20,B_2O_3 6.37,H_2O^+ 1.33,H_2O^- 0.06,total 99.21% corresponding to ( Ca_<l.94>Mn_<0.06>)_<〓2.00> (Fe^<2+>_<0.71>Mg_<0.21>Al_<0.04>Fe^<3+>_<0.01>Ti_<0.01> )_<〓0.98>Al_<2.00>B_<l.04>Si_<4.00>O_<16>H_<0.84> on the basis of total O = 16. The empirical formula of datolite, derived from the chemical analysis, is very close to the ideal formula CaBSiO_5 (OH) with a slight H_2O excess. Idiomorphic forms of the minerals are exclusively found in voids in veins, although partially developed forms of ferroaxinite are common. Ferroaxinite is tabular with largerr(011) and b(010). Datolite idiomorphs are short prisms with m(110) and s(102) dominant. Associated minerals within and adjacent to veins are quartz, calcite, albite, adularia, chlorite, and bannisterite, together with pumpellyite. In veins ferroaxinite always preceeds datolite in the crystallisation sequence. This is similar to the relationship between manganaxinite and datolite in skarns from some pyrometasomatic ore deposits in Kyushu. Some veins lack ferroaxinite and have pumpellyite instead, drawing attention to the fact that, leaving aside minor differences in H_2O content, subtraction of HBO_2 + SiO_2 from the ferroaxinite formula yields pumpellyite-(Fe^<2+>). | |||||||
ISSN | ||||||||
収録物識別子タイプ | ISSN | |||||||
収録物識別子 | 03886298 | |||||||
NII論文ID | ||||||||
関連タイプ | isIdenticalTo | |||||||
識別子タイプ | NAID | |||||||
関連識別子 | 110000413339 | |||||||
NII書誌ID | ||||||||
収録物識別子タイプ | NCID | |||||||
収録物識別子 | AN00103190 | |||||||
フォーマット | ||||||||
内容記述タイプ | Other | |||||||
内容記述 | application/pdf | |||||||
著者版フラグ | ||||||||
出版タイプ | VoR | |||||||
出版タイプResource | http://purl.org/coar/version/c_970fb48d4fbd8a85 |