宁芜矿集区及邻区深部电性结构研究
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摘要
随着浅部矿产资源的勘探开发殆尽,寻找深部矿产资源显得十分必要,深部矿产的形成与深部结构构造关系紧密,深部结构的透明化是深部资源探测的突破口。本文依据近年完成的6条大地电磁测深(MT)剖面数据(L1线(定远—溧阳)、L2线(姑山—江宁)、L3线(巢湖—当涂)、L4线(三山街—南陵)、L5线(鸠江区—高淳)和LY2线(芜湖—铜陵)),应用现代大地电磁数据处理技术及二维非线性共轭梯度算法,对MT数据进行了统一的处理及反演,取得了剖面覆盖区域的上地壳二维电性结构模型。结合研究区重磁不同深度异常特征、重磁多尺度边缘检测结果以及物性资料,对宁芜矿集区及其邻区深部结构进行了讨论,取得了一些新的认识。
数据处理及分析表明：研究区上地壳电性结构可以近似为二维结构,电性主轴方位具有北东、北西两个方向,局部变化范围较大,表明宁芜火山岩盆地构造复杂,具有北东、北西向两个主构造方向。大地电磁测深数据观测最低频至0.0001Hz,满足目标研究深度(-10km)。
二维电性结构模型表明：1.区域上地壳低阻异常带与已知的断裂带基本吻合,不同剖面的交接处电性结构相似,说明反演模型较为可靠。2.宁芜火山岩盆地自南而北具有低—高—低的电性结构特征,剖面南段及北段的低阻体可能是盆地内深断裂的电性反映,中段马鞍山附近巨型高阻体是侵入体的电性反映,照此推测,宁芜矿集区中段深部存在第二找矿空间的可能性不大。3.根据2线高、中、低频率点倾子走向认为宁芜火山岩盆地浅部构造较复杂：倾子方向为北西、北东向兼具,深部构造具有明显的北西向为主的特征。4.巢湖—当涂剖面的电性结构反映了区域的推覆构造特征,认为可能与造山过程中的扬子板块向华北板块俯冲的强挤压变形环境有关；含山附近存在“W”型低阻带,剖面东段的“茄子”状低阻体与姑山—江宁剖面南端的低阻体是同一异常体的电性反映。5.三山街—南陵剖面具有层状的电性结构特征,深部高阻层可能是基底地层的电性反映。6.繁昌盆地深部存在“团块状”低阻体,是繁昌火山岩盆地电性反映。
采用多次匹配滤波技术对区域1：20万重力、航磁数据进行了处理,获得了浅、中、深三个不同深度层次的重磁异常信息,重磁多尺度边缘检测结果表明：1.宁芜盆地重力异常幅值比繁昌盆地低；2.边缘检测线多呈北东向展布,主要反映了区域断裂系统,宁芜火山岩盆地具有高重力异常特征,繁昌盆地局部和繁昌-马鞍山中间局部具有高重力异常的特征；3.宁芜火山岩盆地北部的南京-湖熟断裂和东部的方山-小丹阳断裂,西部的长江断裂和南部的三山-宣城断裂没有明显的异常显示；4.查明了火山岩盆地和岩体(隐伏岩体)的边界。重力及磁性异常同时显示茅山断裂、江南断裂均为切割深度较大的断裂。
As the mineral resources in shallow are nearly developed.It is necessary to explore deep mineral resources.The relationship between deep resources and deep structure is closely,so,the breakthrough of deep resource exploration is the transparency of the deep structure.Based on the magnetotelluric sounding (MT) from six profiles (the line1(Ding Yuan-Li Yang),line2(GuShan-JiangNing district),line3(ChaoHu-),line4(SanShan-NanLing),line5(JiuJiang-GaoChun),line Y2(WuHu-TongLing)) finished by Institute of Mineral Resources Chinese Academy of Geological Sciences and modern data processing technology and two-dimensional algorithm to data inversion,the paper presents a two-dimensional model of upper crust electrical structure in profile-controlled region. Combined with the gravity and magnetic anomalies of different depth and multi-scale edge detectionin and physical data in the study area, some important cognition on deep structure are obtained in NingWu volcanic basin and its adjacent area.
Data processing and analysis show that the upper electrical structure of research area is approximately a two-dimensional structure,in which electrical axis is nearly north-east and north-west direction, partially varies in a large range,and the main strike of deep structure in the NingWu volcanic basin is north-east,north-west. The exploration depth of the lowest frequency (1000s) of MT data achieve-10km enoughly.
Two-dimensional electrical structure model shows that:1.the low-resistivity zone or electrical gradient zone roughly coincides with the major fault line delineated by regional geological data.The electrical structure of different profile in intersection point is approximate,which indicates that the inversion model is reliable;2.The electrical structure in NingWu volcanic basin from south to north is low-high-low,and the low resistivity in south and north is deep fracture,and the high resistivity in Ma'anshan is giant granite. According to this conjecture, the possibility of a second prospecting space existing is lowest;3.According to the tipper strike analysis of high, middle and low frequency shows that the structural trend of deep in NingWu volcanic basin is north-east and shallow is north-east,north-west;4.The electrical structure of ChaoHu-DangTu profile reflects the thrust nappe structure in the study areas,which related to the deformation environment under strong squeezing as the orogenic process of the Yangtze plate subduction beneath the North China plate.5.There exists a low resistivity zone and like "W" in HanShan.The low resistivity like eggplant in the eastern section of profile3is similar to the low resistivity lies in the south of profile2,which is considered to be anomaly induced by the same low resistivity body. Profile from SanShan to NanLing is the characteristic of layered electrical structure.6.There is a massive low resistivity body in the deep of FanChang vicinity,which is thought to be anomaly induced by FanChang volcanic basin.
Regional1:200,000gravity, magnetic data processing based on multiple matched filter technology. Gravity and magnetic anomaly of different depth-shallow, medium and deep is obtained. The results show that:1.the gravity anomaly in NingWu basin is lower than in FanChan basin. Regional gravity, magnetic data processing based on potential field multi-scale edge detection;2.The gravity multi-scale edge detection line mainly spread in the north-eastern direction,which reflects regional fault system.Regional tectonic framework is established.NingWu volcanic basin and part of FanChang volcanic basin and middle of FanChang and Ma'anshan are characteristic of high gravity anomaly;3.The gravity multi-scale edge detection line also shows NanJing-HuShu Fault in the north and FangShan-Xiao Danyang Fault in the east,but there is no obvious anomaly of ChangJiang Fault in the west and SanShan-NanLing Fault in the south;4.Aeromagnetic multi-scale edge detection line reflects the boundary of volcanic basin and concealed rock body.Gravity and magnetic anomaly commonly shows that MaoShan Fault and JiangNan Fault are deep fault.
数据处理及分析表明：研究区上地壳电性结构可以近似为二维结构,电性主轴方位具有北东、北西两个方向,局部变化范围较大,表明宁芜火山岩盆地构造复杂,具有北东、北西向两个主构造方向。大地电磁测深数据观测最低频至0.0001Hz,满足目标研究深度(-10km)。
二维电性结构模型表明：1.区域上地壳低阻异常带与已知的断裂带基本吻合,不同剖面的交接处电性结构相似,说明反演模型较为可靠。2.宁芜火山岩盆地自南而北具有低—高—低的电性结构特征,剖面南段及北段的低阻体可能是盆地内深断裂的电性反映,中段马鞍山附近巨型高阻体是侵入体的电性反映,照此推测,宁芜矿集区中段深部存在第二找矿空间的可能性不大。3.根据2线高、中、低频率点倾子走向认为宁芜火山岩盆地浅部构造较复杂：倾子方向为北西、北东向兼具,深部构造具有明显的北西向为主的特征。4.巢湖—当涂剖面的电性结构反映了区域的推覆构造特征,认为可能与造山过程中的扬子板块向华北板块俯冲的强挤压变形环境有关；含山附近存在“W”型低阻带,剖面东段的“茄子”状低阻体与姑山—江宁剖面南端的低阻体是同一异常体的电性反映。5.三山街—南陵剖面具有层状的电性结构特征,深部高阻层可能是基底地层的电性反映。6.繁昌盆地深部存在“团块状”低阻体,是繁昌火山岩盆地电性反映。
采用多次匹配滤波技术对区域1：20万重力、航磁数据进行了处理,获得了浅、中、深三个不同深度层次的重磁异常信息,重磁多尺度边缘检测结果表明：1.宁芜盆地重力异常幅值比繁昌盆地低；2.边缘检测线多呈北东向展布,主要反映了区域断裂系统,宁芜火山岩盆地具有高重力异常特征,繁昌盆地局部和繁昌-马鞍山中间局部具有高重力异常的特征；3.宁芜火山岩盆地北部的南京-湖熟断裂和东部的方山-小丹阳断裂,西部的长江断裂和南部的三山-宣城断裂没有明显的异常显示；4.查明了火山岩盆地和岩体(隐伏岩体)的边界。重力及磁性异常同时显示茅山断裂、江南断裂均为切割深度较大的断裂。
As the mineral resources in shallow are nearly developed.It is necessary to explore deep mineral resources.The relationship between deep resources and deep structure is closely,so,the breakthrough of deep resource exploration is the transparency of the deep structure.Based on the magnetotelluric sounding (MT) from six profiles (the line1(Ding Yuan-Li Yang),line2(GuShan-JiangNing district),line3(ChaoHu-),line4(SanShan-NanLing),line5(JiuJiang-GaoChun),line Y2(WuHu-TongLing)) finished by Institute of Mineral Resources Chinese Academy of Geological Sciences and modern data processing technology and two-dimensional algorithm to data inversion,the paper presents a two-dimensional model of upper crust electrical structure in profile-controlled region. Combined with the gravity and magnetic anomalies of different depth and multi-scale edge detectionin and physical data in the study area, some important cognition on deep structure are obtained in NingWu volcanic basin and its adjacent area.
Data processing and analysis show that the upper electrical structure of research area is approximately a two-dimensional structure,in which electrical axis is nearly north-east and north-west direction, partially varies in a large range,and the main strike of deep structure in the NingWu volcanic basin is north-east,north-west. The exploration depth of the lowest frequency (1000s) of MT data achieve-10km enoughly.
Two-dimensional electrical structure model shows that:1.the low-resistivity zone or electrical gradient zone roughly coincides with the major fault line delineated by regional geological data.The electrical structure of different profile in intersection point is approximate,which indicates that the inversion model is reliable;2.The electrical structure in NingWu volcanic basin from south to north is low-high-low,and the low resistivity in south and north is deep fracture,and the high resistivity in Ma'anshan is giant granite. According to this conjecture, the possibility of a second prospecting space existing is lowest;3.According to the tipper strike analysis of high, middle and low frequency shows that the structural trend of deep in NingWu volcanic basin is north-east and shallow is north-east,north-west;4.The electrical structure of ChaoHu-DangTu profile reflects the thrust nappe structure in the study areas,which related to the deformation environment under strong squeezing as the orogenic process of the Yangtze plate subduction beneath the North China plate.5.There exists a low resistivity zone and like "W" in HanShan.The low resistivity like eggplant in the eastern section of profile3is similar to the low resistivity lies in the south of profile2,which is considered to be anomaly induced by the same low resistivity body. Profile from SanShan to NanLing is the characteristic of layered electrical structure.6.There is a massive low resistivity body in the deep of FanChang vicinity,which is thought to be anomaly induced by FanChang volcanic basin.
Regional1:200,000gravity, magnetic data processing based on multiple matched filter technology. Gravity and magnetic anomaly of different depth-shallow, medium and deep is obtained. The results show that:1.the gravity anomaly in NingWu basin is lower than in FanChan basin. Regional gravity, magnetic data processing based on potential field multi-scale edge detection;2.The gravity multi-scale edge detection line mainly spread in the north-eastern direction,which reflects regional fault system.Regional tectonic framework is established.NingWu volcanic basin and part of FanChang volcanic basin and middle of FanChang and Ma'anshan are characteristic of high gravity anomaly;3.The gravity multi-scale edge detection line also shows NanJing-HuShu Fault in the north and FangShan-Xiao Danyang Fault in the east,but there is no obvious anomaly of ChangJiang Fault in the west and SanShan-NanLing Fault in the south;4.Aeromagnetic multi-scale edge detection line reflects the boundary of volcanic basin and concealed rock body.Gravity and magnetic anomaly commonly shows that MaoShan Fault and JiangNan Fault are deep fault.
引文
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