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Bulk chemical composition of the Hotokegaura Green Tuff , Hukuura Dacite and Maruyama Rhyolite in western Shimokita Peninsula, Aomori Prefecture

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posted on 2024-05-22, 06:29 authored by Shu Moriai, Yuji Orihashi, Minoru Sasaki, Shogo Numata, Sota Niki, Hisashi Asanuma, Yoshihiro Asahara, Takafumi Hirata

Bulk chemical compositions of the obsidian (OB) from the Hinokigawa Formation (Hinokigawa basin), the pumice of the Hotokegaura Tuff (HT), and the rhyolites of the Fukuura Rhyolite Lava (FR) and Maruyama Rhyolite Lava (MR).

Determined by XRF (Philips PW2400) set in Hirosaki University and LA-ICP-MS (NWR-213+Agilent 7700x) set in Nagoya University. The detail methods were described in Tani et al. (2002) and Orihashi and Hirata (2003), respectively. n.d. = not detected 

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Corresponding author email address

oripachi@hirosaki-u.ac.jp

Manuscript title (in Japanese)

青森県,下北半島西部に分布する新第三系年代層序の再検討と仏ヶ浦カルデラの提唱

Authors (in Japanese)

盛合 秀,折橋裕二,佐々木実,沼田翔伍,仁木創太,浅沼 尚,淺原良浩,平田岳史

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© 2024 The Geological Society of Japan

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    地質学雑誌/The Journal of The Geological Society of Japan

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