Metallogenic Prediction of Magnetite in the Pandian Area at the Northwest Margin of Luxi Uplift, China: Constraints of Wide-Field Electromagnetic Data

• Published in: Remote sensing (Basel, Switzerland) Switzerland), 2023-03, Vol.15 (5), p.1217
• Main Authors: Liu, Jianxin, Zhou, Keke, Liu, Hongda, Guo, Rongwen, Zhu, Yunqi, Zhang, Zihao, Liu, Rong
• Format: Article
• Language: English
• Subjects: Analysis; China; Diorite; Electric contacts; Electric properties; Electrical resistivity; electrical structures; Electromagnetism; Fault lines; Geoelectricity; Geology; Gravity; Isotopes; Limestone; Lithology; Magnetic methods; Magnetism; Magnetite; metallogenic prediction; Methods; Mineral deposits; Mineralization; Minerals; Ordovician; Ore deposits; Overburden; Paleozoic; Pandian deposit; Porphyry; Potential fields; Remote sensing; Rocks; Rocks, Metamorphic; Spatial distribution; Strata; Two dimensional models; Uplift; wide-field electromagnetic method
• ISSN: 2072-4292; 2072-4292
• DOI: 10.3390/rs15051217

The Pandian deposit is a newly discovered contact metasomatic skarn magnetite deposit found in the Cainozoic super-thick overburden on the northwest margin of Luxi Uplift (LXU). Presently, the horizontal scale of the deposit delineated by the potential field (gravity and magnetic method) has shown giant potential for ore deposits, and mapping the ore-controlling structures in the vertical scale becomes a primary task for metallogenic prediction. In our study, the wide-field electromagnetic method (WFEM), with a strong anti-noise ability in recording electromagnetic signals on the surface at multiple frequencies, is applied to characterize the deep conductivity distribution of the Pandian area. Based on the inversion results from two parallel WFEM profiles, which consist of 105 sites and previous geological and geophysical results, the 2D geoelectric models are established. The low-resistivity regions (with a typical range of 25~32 Ω·m) in the electrical models are proven to be ore bodies of Pandian deposit, which are developed along the contact zone between Yanshanian intrusive rocks and Paleozoic Ordovician strata. The scattered bodies (typically >32 Ω·m) in Ordovician limestone strata are probably caused by intrusive diorite pluton closely related to magnetite mineralization. Due to contact metasomatism, bedded limestone near magnetite was metamorphosed into marble and accompanied by low-resistivity skarn alteration, with resistivity much different from its high-resistivity protolith. The inverted geoelectrical models visually reflect the spatial distribution features of intrusive rocks and lithologic alteration/fracture zones.