Fluid inclusions and sulfur stable isotopes of the Sarab 3 iron ore deposit (the Shahrak mining area - north Bijar)
Introduction Cenozoic magmatism in Central Iran has caused formation of contact metmorphed rocks especially skarns (Calagari and Hosseinzadeh, 2006, Karimzadeh Somarain and Moayyed, 2002). The skarns consist of valuable ore deposits. The Shahrak mining area is located on the border of Central Iran...
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| 主要な著者: | , |
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| フォーマット: | Artigo |
| 言語: | Persa |
| 出版事項: |
Ferdowsi University of Mashhad
2021-02-01
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| シリーズ: | Journal of Economic Geology |
| 主題: | |
| オンライン･アクセス: | https://econg.um.ac.ir/article_39855.html?lang=en |
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