Mineralization and trace element distribution in pyrite using EMPA in exploration drill holes from Cheshmeh Zard gold district, Khorasan Razavi Province, Iran
Introduction<br> Pyrite is the most abundant sulfide mineral in low sulfidation ore deposits. Experimental studies have shown that low-temperature (<150°C) pyrite that formed rapidly is more likely to be fine-grained and framboidal in shape compared to pyrite crystals that formed more slow...
Main Authors: | , , |
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Format: | Article |
Language: | fas |
Published: |
Ferdowsi University of Mashhad
2015-10-01
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Series: | Journal of Economic Geology |
Subjects: | |
Online Access: | http://econg.um.ac.ir/index.php/econg/article/view/41616 |