会理市某矿区地层、构造与钒钛磁铁矿特征研究
Journal: Geological and Mineral Surveying and Mapping DOI: 10.12238/gmsm.v8i4.2257
Abstract
本文基于详细的地质勘查资料,系统阐述了攀西某勘查区的地层序列、构造格架及矿化特征。勘查区主要出露南华系澄江组(Nhc)和中元古代通安增生杂岩带(Pt₂)地层,并发育辉长岩、辉石橄榄岩等岩脉。通安杂岩带由基质(板岩、千枚岩)和岩块(白云岩、硅质白云岩、大理岩)组成。勘查区主要以逆断层较为发育。在勘查区内发现钒钛磁铁矿：钒钛磁铁矿体(Ⅰ-Ⅲ号)主要赋存于千枚岩(phy)中,受断层切割；研究揭示了地层—构造—岩浆活动对成矿的控制作用,为区域找矿提供依据。
Keywords
通安增生杂岩带；构造；千枚岩；钒钛磁铁矿
Full Text
PDF - Viewed/Downloaded: 0 TimesReferences
[1] 王登红,李建康,赵正.中国钒钛磁铁矿成矿规律与资源潜力[J].地质学报,2013,87(5):623-641.
[2] Zhou M F,Robinson P T,Lesher C M,et al.Geochemistry, petro genesis and metallogenesis of the Panzhihua gabbroic layered intr usion and associated Fe-Ti-V oxide deposits, Sichuan Province, SW China[J].Journal of Petrology,2005,46(11):2253-2280.
[3] 张招崇,李承东,李立兴.钒钛磁铁矿矿床成矿作用与研究进展[J].岩石学报,2015,31(2):311-326.
[2] Zhou M F,Robinson P T,Lesher C M,et al.Geochemistry, petro genesis and metallogenesis of the Panzhihua gabbroic layered intr usion and associated Fe-Ti-V oxide deposits, Sichuan Province, SW China[J].Journal of Petrology,2005,46(11):2253-2280.
[3] 张招崇,李承东,李立兴.钒钛磁铁矿矿床成矿作用与研究进展[J].岩石学报,2015,31(2):311-326.
Copyright © 2025 何军, 杨延林, 赵刚, 杨然庆
This work is licensed under a Creative Commons Attribution-NonCommercial 4.0 International License