摘要
棉花地钛磁铁矿区位于哀牢山断裂带南部,是欧亚板块与印支板块构造较为发育的部位,由于长期而持续的俯冲挤压,围限于红河断裂和哀牢山断裂之间的哀牢山地体内发育多处铜、铁、金等多金属矿床。从研究地层、构造、岩浆岩、变质作用等特征入手,结合大比例尺野外地质勘查工作,分析矿区找矿前景,以期为后续钛铁矿矿床地质勘查与找矿提供相应的支撑。
The Mianhuadi Titanium Magnetite Mining Area is located in the southern part of the Ailaoshan Fault Zone,where the Eurasian Plate and Indosinian Plate structures are relatively developed.Due to long-term and continuous subduction and compression,multiple polymetallic deposits such as copper,iron,and gold have developed within the Ailaoshan Mountains between the Honghe Fault and the Ailaoshan Fault.Starting from the study of geological features such as stratigraphy,structure,magmatic rocks,and metamorphic processes,combined with large-scale field geological exploration work,analyze the prospecting prospects of the mining area,in order to provide corresponding support for subsequent geological exploration and prospecting of ilmenite deposits.
作者
胡一多
蒋文奎
吴红梅
祝强
尹红淋
Hu Yiduo;Jiang Wenkui;Wu Hongmei;Zhu Qiang;Yin Honglin(Kunming Vocational and Technical College of Industry,Anning,Yunnan 650302;China Railway Construction Bridge Engineering Bureau Group Co.,Ltd.,Tianjin 300191;KISC Honghe Mining Co.,Ltd.,Honghe,Yunnan 661000)
出处
《现代工程科技》
2024年第14期77-80,共4页
Modern Engineering Technology
基金
云南省教育厅科学研究基金项目“基于机器视觉技术的矿山选矿工序能耗监测智能化研究”(2024J1489)。
关键词
哀牢山南段
钛磁铁矿
矿床
找矿
southern section of Ailao Mountain
titanium magnetite
mineral deposit
looking for minerals
