Origin of anomalously Ni-rich parental magmas and genesis of the Huangshannan Ni-Cu sulfide deposit, Central Asian Orogenic Belt, Northwestern China
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- 作者：Yun Zhao ; Chunji Xue ; chunji.xue@cugb.edu.cn" class="auth_mail" title="E-mail the corresponding author ; Xiaobo Zhao ; Yongqiang Yang ; Junjun Ke ; Bo Zu ; Guozhen Zhang
- 关键词：Huangshannan Intrusion ; Ni-rich parental magmas ; Different magma pulses and types ; Olivine compositional variation
- 刊名：Ore Geology Reviews
- 出版年：2016
- 出版时间：September 2016
- 年：2016
- 卷：77
- 期：Complete
- 页码：57-71
- 全文大小：7236 K
文摘
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The Ni-rich parental magmas of the Huangshannan Intrusion are created by a process of upgrading and scavenging of metals from previously formed sulfide melts.
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The Huangshannan Intrusion was formed by multiple magma pulses.
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The parental magma that formed the lherzolite has experienced previous sulfide segregation and olivine crystallization.
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