Magnetotelluric signatures for deep copper exploration in North Xinjiang, China: Revealing controls of deposit type and sulfide content on geophysical responses

IF 4.3 2区 地球科学 Q1 GEOLOGY
Ore Geology Reviews Pub Date : 2026-03-01 Epub Date: 2026-02-06 DOI:10.1016/j.oregeorev.2026.107162
Aolin Pan , Aimin Du , Tiebing Liu , Lei Meng , Changhao Li , Changming Yu
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Abstract

Discriminating deep-seated orebodies across diverse copper deposit types remains a challenge in exploration geophysics, largely due to highly variable sulfide mineralization styles and complex host-rock settings. To address this, we conducted an integrated geological–geophysical study that combines deposit geological models with high-frequency audio magnetotelluric (AMT) surveys using the Stratagem EH4 system. Three representative copper deposits in North Xinjiang, China, were examined: the Ashele deposit (volcanogenic massive sulfide, VMS-type, high-grade massive sulfides), the Hongguleleng deposit (Manto-type, moderate-grade vein-style sulfides), and the Baogutu deposit (porphyry-type, low-grade disseminated sulfides).
Geological cross-sections and laboratory measurements of rock electrical properties were integrated to constrain two-dimensional (2D) inversions of the AMT data. The results reveal distinct resistivity signatures for three deposit types: very low resistivity anomalies (10–100 Ω·m) characterize VMS mineralization, moderate resistivity anomalies (100–300 Ω·m) correspond to Manto-type vein systems, and relatively higher yet significant resistivity anomalies (100–1000 Ω·m) are associated with disseminated porphyry mineralization. Furthermore, a series of concealed resistivity anomalies were delineated adjacent to and beneath known orebodies at all three deposits, identifying promising targets for deep exploration. Based on these findings, we propose three resistivity structural patterns: a “lens-over-feeder” geometry for VMS deposits, a “stratabound conductive slab” for Manto-type deposits, and a “conductive ring” structure for porphyry systems. This integrated geology–geophysics approach provides a practical framework for enhancing the detection and targeting of concealed copper mineralization in North Xinjiang and other similar terrains worldwide.

Abstract Image

新疆北部深部铜矿的大地电磁特征:揭示矿床类型和硫化物含量对地球物理响应的控制
在不同类型的铜矿床中识别深部矿体仍然是勘探地球物理中的一个挑战,这主要是由于硫化物矿化样式的高度变化和复杂的主岩环境。为了解决这个问题,我们进行了一项综合地质地球物理研究,将矿床地质模型与使用Stratagem EH4系统的高频音频大地电磁(AMT)调查相结合。对新疆北部具有代表性的3个铜矿床进行了勘查:阿舍勒铜矿床(火山成因块状硫化物,vms型,高品位块状硫化物)、红古乐冷铜矿床(曼托型,中品位脉状硫化物)和包谷图铜矿床(斑岩型,低品位浸染型硫化物)。将地质剖面和岩石电性的实验室测量结果结合起来,约束AMT数据的二维(2D)反演。结果表明,3种矿床类型具有明显的电阻率特征:极低电阻率异常(10-100 Ω·m)代表VMS矿化特征,中电阻率异常(100-300 Ω·m)代表manto型脉系特征,较高且显著的电阻率异常(100-1000 Ω·m)代表浸染斑岩矿化特征。此外,在三个矿床已知矿体的邻近和下方圈定了一系列隐伏电阻率异常,确定了深部勘探的有利靶区。基于这些发现,我们提出了3种电阻率结构模式:VMS矿床为“透镜-过馈线”结构,manto型矿床为“层控导电板”结构,斑岩体系为“导电环”结构。该方法为加强新疆北部及世界范围内类似地区隐伏铜矿的探测与找矿提供了实用框架。
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来源期刊
Ore Geology Reviews
Ore Geology Reviews 地学-地质学
CiteScore
6.50
自引率
27.30%
发文量
546
审稿时长
22.9 weeks
期刊介绍: Ore Geology Reviews aims to familiarize all earth scientists with recent advances in a number of interconnected disciplines related to the study of, and search for, ore deposits. The reviews range from brief to longer contributions, but the journal preferentially publishes manuscripts that fill the niche between the commonly shorter journal articles and the comprehensive book coverages, and thus has a special appeal to many authors and readers.
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