滇西北烂泥塘斑岩铜金矿床铁氧化物LA-ICP-MS微量元素特征及其地质意义
Trace Elemental Compositions of Iron Oxides from the Lannitang Porphyry Cu-Au Deposit in the Zhongdian Region (Northwest) and the Geological Significances：A LA-ICP-MS Study
（a）（Ti+V）-Ni/（Cr+Mn）；（b）（Ti+V）-（Al+Mn）
滇西北烂泥塘斑岩铜金矿床铁氧化物LA-ICP-MS微量元素特征及其地质意义 |
| 郭剑衡,冷成彪,张兴春,张伟,尹崇军,张陆佳,田振东 |
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Trace Elemental Compositions of Iron Oxides from the Lannitang Porphyry Cu-Au Deposit in the Zhongdian Region (Northwest) and the Geological Significances：A LA-ICP-MS Study |
| Jianheng GUO,Chengbiao LENG,Xingchun ZHANG,Wei ZHANG,Chongjun YIN,Lujia ZHANG,Zhendong TIAN |
| 图11 烂泥塘斑岩铜金矿床磁铁矿成因判别图解[ |
| Fig.11 Discrimination diagram of magnetite genesis in Lannitang porphyry Cu-Au deposit[ （a）（Ti+V）-Ni/（Cr+Mn）；（b）（Ti+V）-（Al+Mn） |
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