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Was the Panzhihua Large Fe-Ti Oxide Deposit,SW China,Formed by Silicate Immiscibility?

DING Xiangli CHEN Xuanhua SHAO Zhaogang

地质学报(英文版)2023,Vol.97Issue(5):1451-1461,11.
地质学报(英文版)2023,Vol.97Issue(5):1451-1461,11.DOI:10.1111/1755-6724.15003

Was the Panzhihua Large Fe-Ti Oxide Deposit,SW China,Formed by Silicate Immiscibility?

Was the Panzhihua Large Fe-Ti Oxide Deposit,SW China,Formed by Silicate Immiscibility?

DING Xiangli 1CHEN Xuanhua 1SHAO Zhaogang1

作者信息

  • 1. Chinese Academy of Geological Sciences,Beijing 100037,China
  • 折叠

摘要

关键词

liquid immiscibility/fractional crystallization/mafic intrusion/Fe-Ti oxide deposit/Panzhihua

Key words

liquid immiscibility/fractional crystallization/mafic intrusion/Fe-Ti oxide deposit/Panzhihua

引用本文复制引用

DING Xiangli,CHEN Xuanhua,SHAO Zhaogang..Was the Panzhihua Large Fe-Ti Oxide Deposit,SW China,Formed by Silicate Immiscibility?[J].地质学报(英文版),2023,97(5):1451-1461,11.

基金项目

This study is co-supported by the China Geological Survey(Grant Nos.DD20230229,DD20190011,DD20221643),and the National Key Research and Development Project of China(Grant No.2018YFC0603701).We appreciate critical comments and constructive suggestions from the two anonymous reviewers that made significant improvements of this manuscript. (Grant Nos.DD20230229,DD20190011,DD20221643)

地质学报(英文版)

OACSCDCSTPCD

1000-9515

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