対馬における銀鉛亜鉛鉱化を伴う高塩素花崗岩の成因
スポンサーリンク
概要
- 論文の詳細を見る
- Society of Resource Geologyの論文
- 2000-09-30
著者
-
Ishihara Shunso
Geological Survey Of Japan Aist
-
Imai Akira
University Of Tokyo
-
Ishihara Shunso
Geological Survey Of Japan
関連論文
- 西南日本の分化チタン鉄鉱系花崗岩類:REE-Sn-W鉱化マグマの起源
- REE Abundance and REE Minerals in Granitic Rocks in the Nanling Range, Jiangxi Province, Southern China, and Generation of the REE-rich Weathered Crust Deposits
- コリア半島地域の中生代-新生代鉱床の硫黄起源の多様性
- 華南の燕山期マグマ性熱水鉱床の硫黄同位体比変化
- REE Mineralization of Weathered Crust and Clay Sediment on Granitic Rocks in the Sanyo Belt, SW Japan and the Southern Jiangxi Province, China
- Resource Evaluation of Indium in the Dajing Tin-Polymetallic Deposits, Inner Mongolia, China
- Chemical Evolution of Zircons in the Paleogene Naegi Granite, Central Japan
- 韓国のカンブロ-オルドヴィス紀炭酸塩岩の硫黄含有量と同位対比:中生代マグマ熱水性鉱床の硫黄起源の可能性
- 韓国の花崗岩類と帯磁率
- 対馬における銀鉛亜鉛鉱化を伴う高塩素花崗岩の成因
- About This Issue and Acknowledgments
- 環太平洋地域顕生代花崗岩類の花崗岩系列と鉱化作用
- ^Ar/^Ar Ages of the Da Lien Granite Related to the Nui Phao W Mineralization in Northern Vietnam
- Tin isotope analysis of cassiterites from Southeastern and Eastern Asia