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The application of tectonogeochemical cuttings survey to gold prospecting in Nanshan area of Danghe, Gansu Province |
ZHAO Ji-Chang( ), FAN Ying, LEI Yi-Lan, YAO Bin-Bin |
Fourth Institute of Geological and Mineral Exploration, Gansu Provincial Bureau of Geology and Mineral Resources,Jiuquan 735000,China |
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Abstract Danghe Nanshan is one of the important gold metallogenic areas in Gansu Province. A number of important gold deposits have been discovered there, such as Jiagongtai, Heicigou and Langchagou, suggesting that the metallogenic conditions are very favorable. However, due to the special geochemical landscape of this area, the peripheral prospecting effect is not good. When carrying out the 1:50 000 mineral prospect survey project in Heidaban-Danghe Nanshan area and aiming at the low and gentle anomalies in the area, the authors introduced the 1:10 000 tectono-geochemical debris survey method into the gold prospecting work for the first time, and analyzed the geochemical characteristics and element combination characteristics in this area. Combined with the metallogenic geological background, 13 comprehensive geochemical anomalies were delineated, and it was found that the main metallogenic elements Au, Pb and Pb and exploration elements As and Sb are intensively enriched in favorable structural positions. Through trenching, 6 new gold mineralization zones were discovered and 15 gold orebodies were delineated. This method was further applied to the gold prospecting in adjacent areas, with good prospecting results achieved. The successful application of this method is of great significance for prospecting in the geochemical landscape area of shallow covered Alpine desert.
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Received: 24 February 2021
Published: 20 August 2021
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Regional geological map of the study area a—geotectonic location of the study area;b—the outcrop of the study area;1—Quaternary modern glaciers;2—Quaternary alluvial proluvial;3—Paleogene Baiyanghe formation;4—Triassic Junzihe Group;5—Permian Nuoyinhe Group;6—Carboniferous Dangheshan formation;7—Devonian-Carboniferous Amunik formation;8—Ordovician Yanchiwan formation;9—Caledonian monzogranite;10—the boundary of unconformity;11—measured reverse fault;12—measured left lateral strike slip fault;13—the fault of unknown nature is measured;14—occurrence of strata;15—gold mine origin (point);16—study area
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Landscape characteristics of the study area
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元素组合 | 异常强度 | 异常面积 S/km2 | 衬度 (K=/T) | 异常NAP值 (K×S) | 浓度分带 | | T | 峰值 | As-21 | 54.3 | 13.21 | 11542 | 90.32 | 4.11 | 371.22 | 内、中、外 | Au-32 | 7.24 | 3.50 | 65.7 | 75.6 | 2.07 | 156.49 | 内、中、外 | Sb-25 | 4.4 | 0.94 | 885.1 | 77.7 | 4.7 | 365.19 | 内、中、外 | W-13 | 1.9 | 1.36 | 4.8 | 49.5 | 1.4 | 69.30 | 中、外 | Sn-27 | 2.5 | 1.79 | 4.6 | 25 | 1.4 | 35.00 | 中、外 | Mo-44 | 1.6 | 1.23 | 2.7 | 11.4 | 1.3 | 14.82 | 外 | Cu-12 | 41.0 | 34.17 | 61.5 | 32.3 | 1.2 | 38.76 | 外 | Pb-34 | 40.9 | 37.18 | 46.3 | 18.3 | 1.1 | 20.13 | 外 |
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Comprehensive anomaly characteristics of AS-7 in 1∶50 000 stream sediment survey
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Analysis of AS-7 comprehensive anomaly in 1∶50 000 stream sediment survey 1—Quaternary system;2—Paleogene Baiyanghe formation;3—Triassic Junzihe Group;4—the upper member of Ordovician Yanchiwan formation;5—Ordovician Tenglong limestone;6—the lower member of Ordovician Yanchiwan formation;7—diorite;8—conformity boundary/unconformity boundary;9—measured reverse fault;10—faults of unknown nature;11—comprehensive abnormality and its number;12—gold producing area and its number
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地层 代号 | 岩性 | 样本数 | Pb | Zn | W | As | Sb | Ag | Au | | | | | | | | | S | Cv | Oyc1 | 变岩屑长石砂岩 粉砂质板岩 | 2136 310 | 23.54 23.42 | 51.77 58.68 | 1.32 1.29 | 22.42 17.71 | 1.11 1.06 | 63.48 86.45 | 7.05 4.58 | 55.84 6.05 | 6.54 3.65 | Otl | 灰岩 变岩屑长石砂岩 | 730 1755 | 45.77 28.91 | 24.56 68.22 | 1.04 1.18 | 10.48 30.18 | 0.93 3.94 | 52.71 89.58 | 3.63 4.52 | 7.12 20.96 | 2.74 4.28 | Oyc2 | 粉砂质板岩 | 1859 | 30.75 | 64.19 | 1.17 | 33.29 | 3.63 | 86.27 | 6.35 | 9.27 | 3.64 | δ | 闪长岩 | 267 | 23.59 | 62.53 | 1.85 | 39.88 | 5.12 | 84.11 | 10.13 | 165.22 | 6.69 |
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Statistical table of element background value in study area
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元素 | 因子序号 | F1 | F2 | F3 | F4 | F5 | F6 | Cu | 0.091 | 0.043 | 0.964 | 0.036 | -0.002 | 0.031 | Pb | 0.861 | 0.006 | -0.023 | -0.101 | 0.305 | 0.096 | Zn | 0.227 | 0.025 | 0.008 | 0.129 | 0.921 | 0.038 | Mo | 0.072 | 0.094 | 0.036 | 0.042 | 0.038 | 0.988 | W | -0.005 | 0.061 | 0.031 | 0.952 | 0.119 | 0.043 | As | 0.254 | 0.759 | -0.092 | 0.217 | -0.186 | 0.059 | Sb | -0.034 | 0.881 | 0.130 | -0.080 | 0.181 | 0.066 | Ag | 0.778 | 0.000 | 0.379 | -0.109 | 0.133 | 0.070 | Au | 0.759 | 0.288 | -0.077 | 0.294 | -0.066 | -0.039 | 方差贡献率/% | 22.805 | 16.113 | 12.302 | 12.092 | 11.627 | 11.163 | 元素组合 | Au、Pb、Ag | As、Sb | Cu | W | Zn | Mo | 备注 | 成矿元素 | 探途元素 | | | | |
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Load matrix of orthogonal rotation factor and information extraction table of factor analysis
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Orthogonal rotation factor load diagram
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Geological map and comprehensive anomaly distribution map of the study area 1—the fifth lithologic member of upper member of Ordovician Yanchiwan formation;2—the fourth lithologic member of the upper member of Ordovician Yanchiwan formation;3—the third lithologic member of the upper member of Ordovician Yanchiwan formation;4—the second lithologic member of the upper member of Ordovician Yanchiwan formation;5—the first lithologic member of upper member of Ordovician Yanchiwan formation;6—Ordovician Tenglong limestone;;7—the first lithologic member of the lower member of Ordovician Yanchiwan formation;8—diorite porphyrite;9—diorite;10—diabase porphyrite;11—gabbro;12—altered fracture zone;13—gold ore body;14—measured reverse fault;15—occurrence of strata;16—Au anomaly;17—As anomaly;18—As anomaly
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异常编号 | 元素组合 | 异常强度 | 异常面积 S/km2 | 衬度 ( K=/T) | 异常NAP值 (K×S) | 浓度分带 | | 峰值 | AR-4 | Au-9 | 226 | 1505 | 0.22 | 41.09 | 9.04 | 内、中、外 | | Ag-8 | 352.3 | 5050 | 0.41 | 5.21 | 2.14 | 内、中、外 | | Sb-7 | 5.28 | 14.47 | 0.013 | 10.34 | 0.13 | 内、中、外 | | Sb-8 | 7.17 | 27.85 | 0.03 | 19.89 | 0.60 | 内、中、外 | | As-7 | 51.98 | 363 | 0.25 | 2.89 | 0.72 | 内、中、外 | | Zn-3 | 167.5 | 1142 | 0.21 | 1.90 | 0.40 | 内、中、外 | | W-2 | 2.28 | 12.23 | 2.59 | 1.42 | 3.68 | 内、中、外 | | Cu-6 | 164.4 | 956 | 0.1 | 4.62 | 0.46 | 内、中、外 | AR-6 | Au-14 | 76.1 | 1084 | 0.47 | 10.95 | 5.15 | 内、中、外 | | Au-18 | 31.3 | 31.3 | 0.02 | 4.5 | 0.09 | 内、中、外 | | Sb-11 | 6.4 | 116.8 | 1.3 | 2.9 | 3.77 | 内、中、外 | | As-15 | 70.3 | 336.8 | 1.2 | 3.4 | 4.08 | 内、中、外 | | W-6 | 8.4 | 20.6 | 0.06 | 6.4 | 0.38 | 内、中、外 | | Ag-45 | 152 | 880 | 0.77 | 1.9 | 1.46 | 中、外 | | Mo-11 | 0.84 | 3.2 | 0.74 | 1.5 | 1.11 | 中、外 | | Mo-10 | 0.74 | 0.94 | 0.05 | 1.4 | 0.07 | 外 | | Cu-3 | 49.4 | 146 | 0.45 | 1.5 | 0.68 | 外 | AR-8 | Au-34 | 268.6 | 2462 | 0.47 | 38.6 | 18.14 | 内、中、外 | | As-35 | 77.5 | 425.5 | 1 | 3.7 | 3.70 | 内、中、外 | | Sb-12 | 5.47 | 19.34 | 0.04 | 3.91 | 0.16 | 内、中、外 | | Sb-29 | 2.64 | 7.68 | 0.09 | 1.88 | 0.17 | 内、中、外 | | Ag-26 | 159.3 | 859 | 0.3 | 1.9 | 0.57 | 中、外 | AR-10 | Au-26 | 35.43 | 1030 | 0.8 | 6.44 | 5.15 | 内、中、外 | | As-22 | 138.12 | 1080 | 0.22 | 7.67 | 1.69 | 内、中、外 | | As-23 | 56.60 | 118 | 0.08 | 3.14 | 0.25 | 内、中、外 | | Sb-17 | 4.24 | 11.79 | 0.13 | 3.03 | 0.39 | 内、中、外 | | Sb-18 | 3.27 | 6.79 | 0.05 | 2.34 | 0.12 | 内、中、外 | | Ag-24 | 106.50 | 438 | 0.22 | 1.58 | 0.35 | 内、中、外 | | Mo-16 | 1.67 | 17.61 | 0.14 | 2.79 | 0.39 | 中、外 | AR-12 | Au-29 | 63.89 | 502 | 0.38 | 11.62 | 4.42 | 内、中、外 | | As-28 | 76.9 | 341.4 | 0.51 | 3.7 | 1.89 | 内、中、外 | | Sb-21 | 2.98 | 11.57 | 0.15 | 2.13 | 0.32 | 内、中、外 | | Sb-24 | 3.53 | 9.03 | 0.11 | 2.52 | 0.28 | 内、中、外 | | W-11 | 3.1 | 4.8 | 0.02 | 2.4 | 0.05 | 外 | | W-12 | 2.3 | 3.7 | 0.03 | 1.8 | 0.05 | 外 | | Mo-12 | 4 | 7.7 | 0.06 | 7.2 | 0.43 | 外 |
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Characteristics of main comprehensive anomalies in the study area
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Rose diagram of anomalous strike in the study area 1—measured reverse fault;2—gold bearing alteration zone
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Characteristics of gold ore bodies in the study area a—surface features of ore bodies; b—altered cataclastic sandstone type gold ore bodies outcrop; c—altered cataclastic diorite type gold ore bodies outcrop; d—outcrops of quartz vein type Au,Ag,Pb and Zn ore bodies
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Comparison of geochemical profiles 1—metalithic arkose;2—diabase;3—gold bearing alteration zone;4—Au content curve;5—As content curve;6—Sb content curve;7—Cu content curve;8—Pb content curve;9—Ag content curve
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