Desilicification and iron activation-reprecipitation in the high-grade magnetite ores in BIFs of the Anshan-Benxi area, China: Evidence from geology, geochemistry and stable isotopic characteristics

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Desilicification and iron activation-reprecipitation in the high-grade magnetite ores in BIFs of the Anshan-Benxi area, China: Evidence from geology, geochemistry and stable isotopic characteristics

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作者：Hou-Min Li^a ; ^{lihoumin2002@163.com" class="auth_mail" title="E-mail the corresponding author} ; Xiu-Qing Yang^a ; Li-Xing Li^a ; Zhao-Chong Zhang^b ; Ming-Jun Liu^c ; Tong Yao^a ; Jing Chen^d
关键词：BIF ; High-grade magnetite ore ; Oxygen and sulfur isotope ; Gongchangling ; Qidashan-Wangjiabuzi ; Anshan-Benxi area
刊名：Journal of Asian Earth Sciences
出版年：2015
出版时间：1 December 2015
年：2015
卷：113
期：part_P3
页码：998-1016
全文大小：4094 K

文摘

•: The G2 and QW iron deposits show different alteration and geochemical features.
•: Desilicification responsible for the high-grade magnetite ores in the G2.
•: Iron activation–reprecipitation generated the high-grade magnetite ores in the QW.

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