Immiscible Fe- and Si-rich silicate melts in plagioclase from the Baima mafic intrusion (SW China): Implications for the origin of bi-modal igneous suites in large igneous provinces
详细信息 查看全文
- 作者：Ping-Ping Liua ; liupingping11@live.cn" class="auth_mail" title="E-mail the corresponding author ; Mei-Fu Zhoua ; Zhongyuan Renb ; Christina Yan Wangc ; Kun Wangc
- 关键词：Melt inclusion ; Liquid immiscibility ; Baima layered mafic intrusion ; Bi-modal igneous suite ; SW China
- 刊名：Journal of Asian Earth Sciences
- 出版年：2016
- 出版时间：1 September 2016
- 年：2016
- 卷：127
- 期：Complete
- 页码：211-230
- 全文大小：6084 K
文摘
- •
Polycrystalline mineral inclusion was firstly identified in plagioclase in the ELIP.
- •
The polycrystalline mineral inclusions represent entrapment of contemporaneous melts.
- •
The trapped melt was likely a mixture of Fe-rich and Si-rich melts with phenocrysts.
- •
Liquid immiscibility shall be considered in the formation of bi-modal igneous suites.