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ニュージーランド北島, オハクネ火口産高マグネシア質安山岩と同質デイサイト(鮫島輝彦先生追悼論文集)
https://doi.org/10.14945/00000323
https://doi.org/10.14945/00000323062a3503-6cc3-4db5-962e-99ed6e80e6f2
名前 / ファイル | ライセンス | アクション |
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KJ00000102357.pdf (644.2 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 | ||||||||
タイトル | ニュージーランド北島, オハクネ火口産高マグネシア質安山岩と同質デイサイト(鮫島輝彦先生追悼論文集) | |||||||
言語 | ||||||||
言語 | jpn | |||||||
キーワード | ||||||||
主題Scheme | Other | |||||||
主題 | island arc | |||||||
キーワード | ||||||||
主題Scheme | Other | |||||||
主題 | mantle peridotite | |||||||
キーワード | ||||||||
主題Scheme | Other | |||||||
主題 | crystal fractionation | |||||||
キーワード | ||||||||
主題Scheme | Other | |||||||
主題 | contamination | |||||||
キーワード | ||||||||
主題Scheme | Other | |||||||
主題 | high-K | |||||||
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 | 10.14945/00000323 | |||||||
ID登録タイプ | JaLC | |||||||
タイトル(別言語) | ||||||||
その他のタイトル | Hight Mg-andesite and -dacite from Ohakune crater, North Island, New Zealand(MEMORIAL VOLUME TO THE LATE PROFESSOR TERUHIKO SAMESHIMA) | |||||||
著者 |
黒田, 直
× 黒田, 直
WEKO
159
× 野村, 忠司× 浦野, 隼臣 |
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書誌情報 |
静岡大学地球科学研究報告 巻 20, p. 41-47, 発行日 1994-03 |
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出版者 | ||||||||
出版者 | 静岡大学地球科学教室 | |||||||
NDC | ||||||||
主題Scheme | NDC | |||||||
主題 | 458 | |||||||
抄録 | ||||||||
内容記述タイプ | Abstract | |||||||
内容記述 | The Ohakune crater is one of the parasitic vents around Ruapehu volcano. Olivine andesite and bronzite dacite occur in and around the crater, the eruption of which took place explosively on the flat laharic plain surrounding Ruapehu volcano. The Ohakune crater rocks ' contain some phenocrysts of Mg-rich olivine (Fo88) or orthopyroxene (En89) , indicating their derivation from the mantle peridotite. The olivine andesites have high contents of MgO (7.3-6.6%) and SiO_2 (55.5-57.4%), similar to magnesian andesites from some island arcs and continental margins. The bronzite dacite also has MgO (5%) despite its relatively high SiO_2 (63.7%). The high-Mg olivine andesites fall near the area of parental basalts and andesites of very low-K and -Rb in the linear trend of the Tongariro volcanic rocks in the K-Rb relation, whereas the high-Mg dacite is plotted on the area of relatively high-K and -Rb in the same linear trend. The dacite may have formed by contamination ( or mixing) of the olivine andesite-forming magma with a high-K and -Rb, felsic crustal material. | |||||||
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 | 110000413344 | |||||||
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 |