Metallogenesis of the sediment-hosted stratiform Cu deposits of the Ravar Copper Belt (RCB), Central Iran

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• 作者：Hassan Azaraien ; ^{h.azaraeen2010@gmail.com} ; Jamshid Shahabpour ^{Shahabpour@yahoo.com} ; Balandeh Aminzadeh ^{aminzadeh85@gmail.com}
• 关键词：Ravar Copper Belt ; Sediment-hosted stratiform copper deposits ; Garedu sandstone ; Spionkopite ; Woody fragments
• 刊名：Ore Geology Reviews
• 出版年：2017
• 出版时间：March 2017
• 年：2017
• 卷：81
• 期：part_P1
• 页码：369-395
• 全文大小：8748 K
• 卷排序：81

文摘

The Ravar copper belt (RCB) was introduced for first time. The RCB is a Cu-Ag-U red bed type sediment-hosted stratiform copper (SSC) belt. Spionkopite as a common supergene mineral in the SSC deposits, is recognized in this belt. Marcasite that was less reported in SSC deposits of the world, is a common mineral in the RCB.