A PALYGORSKITE VEIN FOUND IN CONGLOMERATE OF THE UPPER EOCENE-LOWER OLIGOCENE RIKUBETSU FORMATION IN NORTHEASTERN HOKKAIDO, JAPAN

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概要

• 論文の詳細を見る

• Palygorskite was found as a clay vein in the Futamata area in northeastern Hokkaido, Japan. A light yellowish pink palygorskite vein was observed within a vertical joint in conglomerate of the Upper Eocene-Lower Oligocene Rikubetsu Formation in the Futamata landslide area. The palygorskite is considered to have crystallized from a low-temperature hydrothermal solution related to the volcanic activity of the Lower Oligocene Futamata Andesites.

• 日本粘土学会の論文

著者

• Maeda Hiroyuki

  Department Of Civil And Environmental Engineering Faculty Of Engineering National University Corpora

• Naya Hiroshi

  The Main Office Of Meiji Consultants Co. Ltd.

• MAEDA HIROYUKI

  Sapporo Technology Professional Training College

• FUKUSHIMA YUTAKA

  Terra Research LLC

• YAMAMOTO YASUHIKO

  Mizumoto Construction Engineering Co., Ltd.

• KOHNO MASANORI

  Graduate School of Engineering, National University Corporation Kitami Institute of Technology

• Yamamoto Yasuhiko

  Mizumoto Construction Engineering Co. Ltd.

• Kohno Masanori

  Graduate School Of Engineering National University Corporation Kitami Institute Of Technology

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• A PALYGORSKITE VEIN FOUND IN CONGLOMERATE OF THE UPPER EOCENE-LOWER OLIGOCENE RIKUBETSU FORMATION IN NORTHEASTERN HOKKAIDO, JAPAN
• 北海道北見鉱床区武華鉱山地域の火山活動,熱水変質作用および浅熱水性金銀鉱化作用の関係

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