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J-GLOBAL ID:201502202858859729   Reference number:15A1036322

Genesis of the Nishiasahi basic intrusive complex in the Asahi Mountains prior to the Cretaceous felsic magmatism

白亜紀珪長質火成活動に先行する西朝日複合塩基性岩体の成因
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Volume: 44  Issue:Page: 189-204 (J-STAGE)  Publication year: 2015 
JST Material Number: G0124B  ISSN: 1345-630X  CODEN: GKKABJ  Document type: Article
Article type: 原著論文  Country of issue: Japan (JPN)  Language: JAPANESE (JA)
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Petrogenesis 
Reference (50):
  • 穴田真一,加々島慎一(2008):朝日山地に分布する西朝日複合塩基性岩体の多様性.MAGMA, 89, 17–31.
  • 安藤 勧,志村俊昭(2000):朝日山地周辺に分布する火成岩類の活動ステージ区分と地球化学.日本地質学会第 107 年学術大会講演要旨,157–157.
  • Arakawa, Y., Saito, Y. and Amakawa, H. (2000): Crustal development of the Hida belt, Japan: Evidence from Nd-Sr isotopic and chemical characteristics of igneous and metamorphic rocks. Tectonophys., 328, 183–204.
  • Arth, J. G. (1976): Behavior of trace elements during magmatic processes-A summary of theoretical models and their applications. J. Res. U.S. Geol. Surv., 4, 41–47.
  • 朝日団体研究グループ(1987):朝日山地南西部の地質—その 1.岩石記載と貫入関係—.地球科学,41, 253–280.
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