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Spatial distribution patterns of concealed plutons in the western Zhen’an area based on gravity anomalies |
ZHANG Jin-Ai( ), YANG Yuan( ), ZHANG Lin |
Shaanxi Mineral Resources and Geological Survey, Xi'an 710068, China |
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Abstract The western Zhen'an area enjoys superior ore-forming conditions of tungsten-molybdenum polymetallic deposits. A batch of large and medium-scale tungsten-molybdenum deposits such as Dongyang, Qipangou, Guilingou, Yueheping, and Hetaoping, have been discovered in this area, and they are related to intrusions. To explore tungsten-molybdenum ore bodies, it is necessary to carry out studies on intrusions related to mineralization, especially concealed intrusions. Based on high-precision gravity anomalies, this study extracted the gravity anomaly data of concealed plutons using the minimum curvature potential field separation method. Moreover, it investigated the plane positions of the concealed plutons in the western Zhen'an area by combining the geophysical characteristics of the exposed plutons, identifying five concealed plutons, namely Lanbandeng, Shapingcun, Yuehetai, Dongchuanjie, and Huangjinmei, through investigation. Moreover, this study conducted the 3D gravity anomaly inversion for typical concealed plutons, determining the spatial distribution characteristics of the concealed plutons. The Yuehetai and eastern Lanbandeng concealed plutons have been verified through boreholes, with high-grade wolframite being discovered. The method proposed in this study can provide technical support for the study of concealed plutons in the Zhen'an area and other areas, as well as important data for the study of the tectonic-magmatic-metallogenic evolution of the southern Qinling metallogenic belt.
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Received: 21 September 2022
Published: 05 July 2023
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Regional geological map of the study area[17]
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地层及 岩(矿)石 | 岩性 | 标本 数量 | 密度ρ/(g·cm-3) | 最大值 | 最小值 | 常见值 | 沉积岩 | 白云岩 | 56 | 3.01 | 2.63 | 2.77 | 灰岩 | 123 | 2.93 | 2.58 | 2.72 | 变砂岩 | 170 | 2.99 | 2.40 | 2.70 | 变质岩 | 大理岩 | 186 | 2.91 | 2.45 | 2.76 | 片岩 | 130 | 2.96 | 2.58 | 2.71 | 板岩 | 22 | 3.11 | 2.53 | 2.72 | 千枚岩 | 10 | 2.78 | 2.63 | 2.71 | 中酸性 岩体 | 闪长岩 | 16 | 2.78 | 2.65 | 2.70 | 石英闪长岩 | 36 | 2.80 | 2.46 | 2.64 | 二长闪长岩 | 36 | 2.73 | 2.60 | 2.65 | 二长花岗岩 | 110 | 2.80 | 2.50 | 2.60 | 花岗岩 | 15 | 2.61 | 2.41 | 2.55 | 矿化体、 岩脉 | 白钨矿化石英脉 | 15 | 2.91 | 2.59 | 2.82 | 白钨矿化白云岩 | 17 | 2.86 | 2.68 | 2.74 | 辉钼矿钼矿 | 16 | 3.15 | 2.57 | 2.86 | 褐铁矿化岩石(脉) | 74 | 2.99 | 2.42 | 2.69 | 石英脉 | 25 | 2.90 | 2.48 | 2.64 |
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Statistical of physical properties of rock and ore specimens in the study area
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Comparison of Bouguer gravity anomaly separation a—Bouguer gravity anomaly;b—residual Bouguer gravity anomaly;c—regional Bouguer gravity anomaly
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Geological and gravity anomaly characteristics of Gaoqiao and Jiangkou rock masses a—geological features;b—Bouguer gravity anomaly;c—residual Bouguer gravity anomaly
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Geological and gravity anomaly characteristics of Laibandeng rock masses a—geological features;b—Bouguer gravity anomaly;c—residual Bouguer gravity anomaly
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Plane distribution map of concealed and semi-concealed rock mass in the study area
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Inferred fault structure distribution map of the study area
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Plane distribution and 3D inversion range of rock mass in the study area
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3D inversion model diagram of rock mass
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