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このアイテムのファイル:
| ファイル | 記述 | サイズ | フォーマット | |
|---|---|---|---|---|
| mfskugm 038001_155.pdf | 231.31 kB | Adobe PDF | 見る/開く |
完全メタデータレコード
| DCフィールド | 値 | 言語 |
|---|---|---|
| dc.contributor.author | Ueda, Tateo | en |
| dc.contributor.alternative | ウエダ, タテオ | ja |
| dc.contributor.transcription | ウエダ, タテオ | ja-Kana |
| dc.date.accessioned | 2014-05-01T05:39:16Z | - |
| dc.date.available | 2014-05-01T05:39:16Z | - |
| dc.date.issued | 1971-08-15 | - |
| dc.identifier.issn | 0454-7810 | - |
| dc.identifier.uri | http://hdl.handle.net/2433/186573 | - |
| dc.description.abstract | Several specimens of dolomite covering those of hydrothermal origin as well as of sedimentary origin have been examined. Content of FeCO3 in specimens of hydrothermal origin is usually high. In specimens which are hydrothermal origin and high in FeCO3 content, hkl reflexions utterly disappear when h+k+l=2n+1 and h=k or k=l or l=h, showing that space group turns from R3 to R3c. The elevation of symmetry may be attributed to a disordering of cations, Ca2+, Mg2+ and Fe2+. | en |
| dc.format.mimetype | application/pdf | - |
| dc.language.iso | eng | - |
| dc.publisher | 京都大学理学部 | ja |
| dc.publisher.alternative | [Faculty of Science, Kyoto University] | en |
| dc.subject.ndc | 450 | - |
| dc.title | Disordering of the Cations, Ca2+, Mg2+, Fe2+ in Dolomite Lattice | en |
| dc.type | departmental bulletin paper | - |
| dc.type.niitype | Departmental Bulletin Paper | - |
| dc.identifier.ncid | AA00732831 | - |
| dc.identifier.jtitle | Memoirs of the Faculty of Science, Kyoto University. Series of geology and mineralogy | en |
| dc.identifier.volume | 38 | - |
| dc.identifier.issue | 1 | - |
| dc.identifier.spage | 155 | - |
| dc.identifier.epage | 161 | - |
| dc.textversion | publisher | - |
| dc.sortkey | 06 | - |
| dcterms.accessRights | open access | - |
| dc.identifier.pissn | 0454-7810 | - |
| 出現コレクション: | Vol. 38 No. 1 | |
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