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モンゴル,ウランバートル・テレーンの石炭紀礫岩中のグラノファイア礫(予報)
https://doi.org/10.18999/bulnum.023.02
a22cbd83-ce18-4a7e-9791-dc242f6811b0
名前 / ファイル | ライセンス | アクション | |
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Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||
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公開日 | 2009-09-16 | |||||
タイトル | ||||||
タイトル | モンゴル,ウランバートル・テレーンの石炭紀礫岩中のグラノファイア礫(予報) | |||||
その他のタイトル | ||||||
その他のタイトル | A petrographical note on granophyre cobble from the Carboniferous conglomerate in the Ulaanbaatar Terrane, central Mongolia | |||||
著者 |
足立, 守
× 足立, 守× ADACHI, Mamoru× 吉田, 英一× YOSHIDA, Hidekazu× 束田, 和弘× TSUKADA, Kazuhiro× DORJSUREN, Bayambadash× SERSMAA, Gonchigdorj× MAJIGSUREN, Uondon× MINJIN, Chuluun |
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抄録 | ||||||
内容記述 | A granophyre cobble was found from conglomerate of the early Carboniferous Altan Ovoo Formation in the Ulaanbaatar Terrane, central Mongolia. The conglomerate occurs in sandstoneshale alternations, is partly matrix-supported and partly clast-supported, and consists largely of rounded pebbles and cobbles of rhyolite with lesser amounts of quartz porphyry, sandstone, mudstone, granite, andesite and granophyre. Clast imbrication, although not common, shows their derivation from the west. The granophyre clast is characterized by having micrographic texture, titanite and secondary pumpellyite. One quartz porphyry clast contains pumpellyite and rock fragments of granophyre very similar to the granophyre clast, suggesting that the granophyre and quartz porphyry are likely to be related in their provenance. |
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内容記述タイプ | Abstract | |||||
出版者 | ||||||
出版者 | 名古屋大学博物館 | |||||
言語 | ||||||
言語 | jpn | |||||
資源タイプ | ||||||
資源 | http://purl.org/coar/resource_type/c_6501 | |||||
タイプ | departmental bulletin paper | |||||
ID登録 | ||||||
ID登録 | 10.18999/bulnum.023.02 | |||||
ID登録タイプ | JaLC | |||||
ISSN(print) | ||||||
収録物識別子タイプ | ISSN | |||||
収録物識別子 | 1346-8286 | |||||
書誌情報 |
名古屋大学博物館報告 巻 23, p. 13-20, 発行日 2007-12-25 |
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フォーマット | ||||||
application/pdf | ||||||
著者版フラグ | ||||||
値 | publisher | |||||
URI | ||||||
識別子 | http://hdl.handle.net/2237/12209 | |||||
識別子タイプ | HDL |