The sources of ore-forming material in the low-sulfidation epithermal Wulaga gold deposit, NE China: Constraints from S, Pb isotopes and REE pattern
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- 作者：Yongbin Wang ; wangyongbin@mail.iggcas.ac.cn" class="auth_mail" title="E-mail the corresponding author ; Qingdong Zeng ; Lingli Zhou ; Shaoxiong Chu ; Yunpeng Guo
- 关键词：Sulfur isotope ; Lead isotope ; REE ; Wulaga gold deposit ; NE China
- 刊名：Ore Geology Reviews
- 出版年：2016
- 出版时间：July 2016
- 年：2016
- 卷：76
- 期：Complete
- 页码：140-151
- 全文大小：6010 K
文摘
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The Wulaga deposit is a granodioritic porphyry-hosted, low-sulfidation epithermal gold deposit
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The sulfur isotopes imply that the sulfur was derived mainly from magmatic volatiles
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The lead isotopes imply that the lead was related to the parent magma of the granodioritic porphyry
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The REE pattern may reflect that the REE were mainly inherited from the granodioritic porphyry.