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  1. 050 理学部
  2. 10 学術雑誌論文
  3. 10 査読済論文
  1. 0 資料タイプ別
  2. 01 学術雑誌論文

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/10191/17767
ad88b389-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 ZA_52(3)_253-267.pdf (2.3 MB)
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
言語 en
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
言語 jpn
資源タイプ
資源 http://purl.org/coar/resource_type/c_6501
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

WEKO 40895

周藤, 賢治

Search repository
茅原, 一也

× 茅原, 一也

WEKO 40896

茅原, 一也

Search repository
著者別名
識別子 40897
識別子Scheme WEKO
姓名 Shuto, Kenji
著者別名
識別子 40898
識別子Scheme WEKO
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
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
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