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Application study of high precision aero magnetic to Wafangdian diamond deposit exploration in Liaoning Province |
AN Zhan-Feng(), JIA Zhi-Ye(), WANG Meng |
China Aero Geophysical Survey and Remote Sensing Center for Natural Resources, Beijing 100083, China |
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Abstract Wafangdian region is an important diamond ore concentration area in Liaoning privence of china, and the metallogenic mother rock is mainly kimberlite. Based on the 1∶10 000 high-precision aeromagnetic data in Wafangdian region, combined with the regional geological background and rock magnetic characteristics, this paper analyzes and summarizes the aeromagnetic anomaly characteristics of the kimberlite. It is found that the distribution direction and shape of the kimberlite rock are mainly controlled by the NEE and NE faults. Generally, the magnetism of kimberlite is strong, which is quite different from that of surrounding rock. The kimberlite corresponds to the NEE-trending isolated aeromagnetic anomaly, and the shape is mostly elliptical. The anomaly amplitude is not greater than 50 nT, and the anomaly distribution range is greater than the exposed area of rock mass. Aeromagnetic anomalies have important indicative significance for the prospecting of kimberlite, which can be used to guide the next geological prospecting deployment.
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Received: 05 December 2021
Published: 28 June 2022
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Corresponding Authors:
JIA Zhi-Ye
E-mail: anzhanfeng@mail.cgs.gov.cn;jiazhiye@mail.cgs.gov.cn
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Geological sketch of Wafangdian region 1—Cenozoic; 2—Mesozoic; 3—Paleozoic; 4—Neoproterozoic Sinian series; 5—Neoproterozoic Nanhua series; 6—Neoproterozoic Qingbaikou series; 7—Paleoproterozoic; 8—Archean gneiss; 9—middle acid intrusive body; 10—diorate porphyrite; 11—dolerite; 12—fault; 13—kimberlite and ore belt number; 14—diamond ore belt section line and marking; 15—scope of diamond ore belt; 16—study aera
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岩性 分类 | 岩性 | 地质 单元 | κ/10-5 SI | | Jr/(10-3 A·m-1) | 变化范围 | 均值 | 均值 | 沉积岩 | 粉砂岩 | K1p | 20~44 | 33 | | | 灰岩 | 2z | 7~25 | 13 | | | | 粉砂质页岩 | 1-2m | 21~42 | 30 | | | | 灰岩 | 1-2m | 19~31 | 25 | | | | 粉砂岩 | Qbq | 4~7 | 5 | | | | 泥灰岩、粉砂岩 | Qbn | 6~49 | 30 | | | | 石英砂岩 | Qbd | 1~18 | 7 | | | | 长石石英砂岩 | Qby | 17~41 | 27 | | | 变质岩 | 斜长角闪岩 | Ar | 7034~13864 | 11013 | | 1500 | 黑云角闪片麻岩 | 1438~5820 | 2171 | 黑云斜长片麻岩 | 16~724 | 146 | 侵入岩 | 斑状金云母金伯利岩 | χσ | 2172~18789 | 6872 | | 155 | 强碳酸盐化金伯利岩 | χσ | 81~243 | 149 | | 80 | 辉绿岩 | βμ | 1025~6508 | 2383 | | 710 | 橄榄玄武岩 | δβ | 1114~3687 | 2046 | | 400 | 角闪质安山岩 | φοα | 1015~4640 | 2824 | | 860 | 闪长玢岩 | δμ | 348~1174 | 679 | | 1140 | 闪长岩 | δ | 102~2984 | 1389 | | 670 | 流纹斑岩 | γπ | 2~17 | 6 | | 160 |
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Statistical table of magnetic parameters of rocks in the study area
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Reduction-to-the-pole of aeromagnetic ΔT anomalies map in Wafangdian region
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岩体 | 航磁异常 | 岩体规模 | 异常幅值/nT | 飞行高度/m | 17号 | (50~180) m×0.43 m | 16 | 119 | 21号 | (20~40) m×1 m | 13 | 123 | 30号 | 245 m×112 m | 39 | 100 | 42号 | 大管355 m×230 m 小管200 m×60 m | 71 | 119 | 50号 | 275 m×55 m | 12 | 61 | 71号 | (4~20) m×0.15 m | 9 | 137 | 75号 | 100 m×0.2 m | 15 | 172 | 91号 | 10 m×0.4 m | 18 | 109 |
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Statistical table of aeromagnetic anomalies of the discovered kimberley rock in Wafangdian region
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Aeromagnetic anomaly characteristics of kimberlite in Liaotiangou area 1—location and number of kimberlite; 2—aeromagnetic inferred fracture;a—aeromagnetic ΔT anomalies contour map; b—aeromagnetic vertical gradient contour map
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Aero-magnetic anomaly characteristics of No.48, No.75 kimberley rock 1—location and number of kimberlite; 2—aeromagnetic inferred fracture;a—aero-magnetic ΔT anomalies contour map; b—aeromagnetic vertical gradient contour map
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