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新潟油・ガス田地域における中新世中～後期の塩基性火山岩
http://hdl.handle.net/10191/17767
http://hdl.handle.net/10191/17767ad88b389-cdfd-4af5-ab0d-65f1740b8311
| 名前 / ファイル | ライセンス | アクション |
|---|---|---|
ZA_52(3)_253-267.pdf (2.3 MB)
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| Item type | 学術雑誌論文 / Journal Article(1) | |||||
|---|---|---|---|---|---|---|
| 公開日 | 2012-04-11 | |||||
| タイトル | ||||||
| タイトル | 新潟油・ガス田地域における中新世中～後期の塩基性火山岩 | |||||
| タイトル | ||||||
| タイトル | 新潟油・ガス田地域における中新世中～後期の塩基性火山岩 | |||||
| 言語 | en | |||||
| 言語 | ||||||
| 言語 | jpn | |||||
| 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 | journal article | |||||
| その他のタイトル | ||||||
| その他のタイトル | Basic Volcanic Rocks of Middle to Late Miocene Ages in the Niigata Oil and Gas Field, Northeast Japan | |||||
| 著者 |
周藤, 賢治
× 周藤, 賢治× 茅原, 一也 |
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| 著者別名 | ||||||
| 識別子Scheme | WEKO | |||||
| 識別子 | 40897 | |||||
| 姓名 | Shuto, Kenji | |||||
| 著者別名 | ||||||
| 識別子Scheme | WEKO | |||||
| 識別子 | 40898 | |||||
| 姓名 | Chihara, Kazuya | |||||
| 抄録 | ||||||
| 内容記述タイプ | Abstract | |||||
| 内容記述 | The "Miocene Regional Basalts", proposed here by the authors, include basalts and dolerites of the Nishikurosawa and Onnagawa stages, which are widely distributed from Aomori through Yamagata to Niigata oil and gas along the Japan Sea coast. Some of these basalts play an important role as oil and gas reservoir. In the present paper, we describe occurrence, mineral chemistry and bulk chemistry of basaltic rocks in the Niigata oil and gas field, especially in the Yahiko-Kakuda area and the Higashiyama area. Systematic lateral variations in the chemical composition of the Miocene Regional Basalts are not observed on the basis of the petrochemical characters of these basalts, including basaltic rocks of the Niigata oil and gas field and those from other localities in Yamagata, Akita and Aomori Prefectures. The Miocene Regional Basalts are composed of not only the island arc-type tholeiite but tholeiitic and alkali basalts which are rich in TiO_2 and/or P_2O_5 and similar in composition to basalts of the oceanic region. It may be possible that such tholeiitic and alkali basalts of oceanic-type were derived from an upper mantle material different from the present upper mantle material in Northeast Japan arc. The origin of these basaltic magma might be derived from a mantle diapir in the same constitution as that of Iceland volcanic. The middle Miocene volcanics of the island arc-type tholeiite and of calc-alkaline series in Northeast Japan arc may have its orig1n in relation to partial melting of upper mantle and lower crust owing to the supply of heat from the ascending mantle diapir. | |||||
| 書誌情報 |
石油技術協会誌 en : 石油技術協会誌 巻 52, 号 3, p. 253-267, 発行日 1987-05 |
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| 出版者 | ||||||
| 出版者 | 石油技術協会 | |||||
| ISSN | ||||||
| 収録物識別子タイプ | ISSN | |||||
| 収録物識別子 | 03709868 | |||||
| 書誌レコードID | ||||||
| 収録物識別子タイプ | NCID | |||||
| 収録物識別子 | AN00130976 | |||||
| 権利 | ||||||
| 権利情報 | 石油技術協会 | |||||
| 著者版フラグ | ||||||
| 値 | publisher | |||||
