Chemical compositions of garnet and clinopyroxene and their genetic significances in Yemaquan skarn iron–copper–zinc deposit, Qimantagh, eastern Kunlun

• Published in: Journal of geochemical exploration Vol. 158; pp. 143 - 154
• Main Authors: Zuo, Pengfei, Liu, Xuefei, Hao, Jinhua, Wang, Yashuai, Zhao, Rui, Ge, Songsheng
• Format: Journal Article
• Language: English
• Published: Elsevier B.V 01.11.2015
• Subjects: Mineralization zonation; Prograde skarns; Skarn iron–copper–zinc deposit; Skarn zonation; Yemaquan; Skarn iron–copper–zinc deposit; Skarn zonation; Yemaquan; Prograde skarns; Mineralization zonation

The Yemaquan skarn deposit in the northwestern part of the Qimantagh is located in the eastern Kunlun orogenic belt. The deposit is hosted in carbonate rocks, siltstones, and sandstones of the Cambrian–Ordovician Tanjianshan Group and Late Carboniferous Di'aosu Formation. These rocks are intrud...