Study on the prospecting model of concealed MVT lead-zinc deposits in northeastern Yunnan Province: A case study of Maozu lead-zinc deposit
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摘要:
滇东北地区是我国MVT型铅锌矿床的重要集中产出地之一,区内浅表资源经长时间开采而逐渐枯竭,亟需在已知矿床的外围及深部寻找到新的接替资源。本文以区内典型的巧家县茂租铅锌矿床为例,通过在矿区已知矿床点开展综合找矿方法试验,并结合前人对本区地质背景、成矿模式、矿床特征、找矿标志等的认识,对本区MVT型铅锌矿床深部找矿的勘查模式进行了研究。研究表明,岩石地球化学测量中沿断层破碎带浓集的Pb-Zn-Ag元素高值异常指示了其深部具备成矿热液活动“痕迹”,音频大地电磁法能够查明地下深部有利赋矿层位(震旦系灯影组和寒武系筇竹寺组)的顶底界面埋深和导(控)矿断层的倾向、规模等地质成矿“格架”背景,面积性激电中梯测量能够在“横向平面尺度”圈定出有利的找矿靶区(高极化异常区),大比例尺激电测深剖面能够在“纵向空间尺度”定位矿(床)体位置(低电阻率、高极化异常体),通过深浅结合的组合勘查技术方法(浅表化探组合元素异常+电阻率剖面深部地质结构+平、剖面激电异常体),可以从多学科交叉的角度为深部找矿靶区优选提供证据支撑。据此,本文提出了“构造地球化学+多维度电法勘探”的勘查模式,此模式有望推广到滇东北铅锌成矿带内的其他铅锌矿区进行找矿示范应用。
Abstract:Northeast Yunnan Province is one of the most important production areas of MVT lead-zinc deposits in China. In recent years, with the gradual depletion of resources in shallow mining areas, it is urgent to find new replacement resources in the peripheral and deep parts of mining areas. Taking the typical MVT Maozu lead-zinc deposit in Qiaojia county as an example, this paper puts forward a prospecting model suitable for deep exploration of MVT lead-zinc deposits in this area. This prospecting model is based on comprehensive exploration methods tests of known deposits around the mining area and detailed study of the geological background, metallogenic model, deposit characteristics, and prospecting indicators of MVT deposits in this area. The experimental data show that the high-value Pb-Zn-Ag anomalies concentrated along the fault fracture zone in the geochemical survey indicate that there are signatures of ore-forming hydrothermal activity in the deep parts of the faults. The audio frequency magnetotelluric method can be used to identify the burial depth of concealed orebodies, the fluctuations in favorable ore-forming interfaces between the Ediacaran Dengying Formation and the Cambrian Qiongzhusi Formation in the deep underground, and the tendency and scale of the ore-forming faults. The intermediate gradient IP (Induced Polarization Method) measurement of an area can delineate the favorable prospecting area (high polarization anomaly area) on the “horizontal plane scale”, and large-scale IP sounding profiles can further delineate the favorable ore body target areas that are of low resistivity and high polarization anomaly on the “vertical space scale”. The research results show that the combined use of the shallow and deep exploration technologies described in this paper, including the combined element anomalies of shallow geochemical exploration, the deep geological structure of the resistivity profile, and the IP anomaly bodies of the plane and profile, can provide interdisciplinary evidence support for optimizing the deep prospecting target area in this area, and the turning points of anticline and syncline folds close to ore-guiding (controlling) faults and the stratigraphic interface of the Dengying Formation and the Qiongzhusi Formation are preferred drilling verification locations.
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Key words:
- Northeast Yunnan /
- MVT-type /
- lead zinc deposit /
- Maozu mining area /
- deep prospecting method /
- prospecting target
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图 1 滇东北大型矿集区铅锌(银)矿床分布示意图(据荣惠锋等,2013编绘)
Figure 1.
图 3 茂租矿区铅锌典型矿床特征(据贺胜辉等, 2006编绘)
Figure 3.
图 2 茂租铅锌矿区地质构造简图(据金灿海等, 2015编绘)
Figure 2.
图 12 滇东北成矿带MVT型铅锌矿床找矿模型图(据李小清, 2013绘编)
Figure 12.
表 1 研究区主要岩(矿)石地层的电性参数统计表
Table 1. Statistical data of electrical parameters of the main rock (ore) strata in the study area
地层名称 地层
代号厚度
(m)岩性 极化率(%) 电阻率(Ω·m) 电性特征分类 均值 变化范围 均值 变化范围 寒武系上统二道水组 ∈3e 154~296 白云岩 0.7 0.37~1.77 965 586~ 2964 高电阻率、低极化率 寒武系中统西王庙组 ∈2x 150~298 白云岩 0.6 0.27~1.07 1512 1622 ~3469 寒武系中统陡坡寺组 ∈2d 32 白云岩 1.1 1.1 1947 1947 页岩、粉砂岩 0.6 0.12~1.35 372 325~425 中高电阻率、低极化率 寒武系下统龙王庙组 ∈1l >300 泥质页岩 0.2 0~0.47 193 45~385 白云岩 0.5 0.12~1.95 1426 819~ 2345 寒武系下统沧浪铺组 ∈1c 140~179 砂页岩 0.2 0~0.35 261 111~735 低电阻率、低极化率 寒武系下统筇竹寺组 ∈1q 150~260 页岩 1.2 0.25~8.35 87 19~223 泥质粉砂岩 0.4 0~1.19 353 114~967 含黄铁矿砂页岩 14.05 14.05 217 217 低电阻率、高极化率 震旦系上统灯影组上段 Z2d2 >500 方铅矿石 7.8 2.9~18.2 9.7 3~20 闪锌矿石 12 8.5~15.7 1070.6 165~ 2954 铅锌硫化矿 15 9.4~40 148.4 51~481 裂隙矿 1.2 0.59~2.63 545 254~824 白云岩 0.55 0~1.51 1841 1088 ~2695 高电阻率、低极化率 震旦系上统灯影组下段 Z2d1 323~663 角砾岩 1.12 0.87~1.54 1533 1277 ~1850 -
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