The behavior of rare-earth elements, zirconium and hafnium during magma evolution and their application in determining mineralized magmatic suites in subduction zones: Constraints from the Cenozoic belts of Iran

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• 作者：Hemayat Jamali ^{hemayatjamali@yahoo.com h.jamali@sci.ui.ac.ir}
• 关键词：Geochemistry of trace elements ; Magma evolution ; Mineralized magmatic suites ; Subduction zone ; Iran
• 刊名：Ore Geology Reviews
• 出版年：2017
• 出版时间：March 2017
• 年：2017
• 卷：81
• 期：part_P1
• 页码：270-279
• 全文大小：2617 K
• 卷排序：81

文摘

Geochemical variations of trace elements (REE, Zr, Hf) have been attributed to subduction processes and arc maturity. Chondrite normalized REE pattern, Zr-Hf and (Zr/Hf)-Hf scatter plots can be used as a tool to recognize the fertile and/or mineralized magmatic suites in magmatic arcs. The geochemistry of trace elements have been attributed to:- Subduction processes- Arc maturity- Recognition of mineralized bodies