东天山白石泉矿区地球物理多方法联合探查与隐伏铜镍矿定位预测
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摘要
隐伏矿床(体)空间位置、形态和矿化强度的预测是经济地质学的前沿课题和热点问题。在新疆东天山白石泉基性-超基性岩型隐伏铜镍矿预测与找矿研究过程,尝试性引入高分辨率的浅层地震与大地电磁测深(MT)方法,并结合常规的高精度重力、磁法和激电,开展隐伏含矿岩体(铜镍矿)空间分布位置、形态和矿化强度的联合探查与定位预测。基本查明了白石泉杂岩体的深部产状与形态结构,发现了5个隐伏低阻异常区。对其中两个低阻异常区的钻探结果表明预测结果是准确的,在异常YC-II位置发现了厚28m的铜镍矿体。
The prediction of the spatial location,shape and mineralization degree of buried ore deposits(orebodies)is a frontier subject and a hot topic of economic geology.An attempt has been made to use the high-resolution shallow-level seismic and magnetotelluric methods,combined with the conventional high-precision gravity,magnetic and induced polarization methods to detect and predict the spatial location,shape and mineralization degree of buried ore-bearing mafic-ultramafic bodies(Cu-Ni deposits)during the prediction and search of the Baishiquan basic-ultrabasic type buried Cu-Ni deposit,eastern Tianshan,Xinjiang.As a result,the deep attitude and shape of the Baishiquan complex are in the main ascertained and five buried low-resistivity anomaly areas were found.Drilling of two of the five anomalies reveals that the results of the prediction by the combined geophysical methods are accuraite and effective and a 28 m thick Cu-Ni orebody is found at the location of anomaly YC-II.
The prediction of the spatial location,shape and mineralization degree of buried ore deposits(orebodies)is a frontier subject and a hot topic of economic geology.An attempt has been made to use the high-resolution shallow-level seismic and magnetotelluric methods,combined with the conventional high-precision gravity,magnetic and induced polarization methods to detect and predict the spatial location,shape and mineralization degree of buried ore-bearing mafic-ultramafic bodies(Cu-Ni deposits)during the prediction and search of the Baishiquan basic-ultrabasic type buried Cu-Ni deposit,eastern Tianshan,Xinjiang.As a result,the deep attitude and shape of the Baishiquan complex are in the main ascertained and five buried low-resistivity anomaly areas were found.Drilling of two of the five anomalies reveals that the results of the prediction by the combined geophysical methods are accuraite and effective and a 28 m thick Cu-Ni orebody is found at the location of anomaly YC-II.
引文
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[2]程裕淇,陈毓川,赵一鸣.初论矿床的成矿系列问题[J].中国地质科学院院报,1979,1(1):32～57.Cheng Yuqi,Chen Yuchuan,Zhao Yiming.Preliminary discussion on the problems of minerogenetic series of mineral deposits[J].Acta Geosicientia Sinica,1979,1(1):32～57(in Chinese with English abstract).
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[8]邓军,翟裕生,杨立强.论剪切带构造成矿系统[J].现代地质,1998,12(4):493～500.Deng Jun,Zhai Yusheng,Yang Liqiang.On ore forming system of shear zone tectonics[J].Geoscience,1998,12(4):493～500(in Chinese with English abstract).
[9]Taylor H P J.The application of oxygen and hydrogen isotope stud-ies to problems of hydrothermal alteration and ore deposition[J].Economic Geology,1974,(69):843～883.
[10]李惠.金矿床地球化学异常模式研究的新进展[J].地质与勘探,1997,33(2):43～47.Li Hui.The new development in geochemical anomaly models of gold deposit[J].Geology and Prospecting,1997,33(2):43～47(in Chinese with English abstract).
[11]姚敬金,曹洛华,张素兰,等.中国大型有色金属贵金属地球物理地球化学找矿模型[M].北京:地质出版社,2002,1～330.Yao Jingjin,Chao Luohua,Zhang Sulan,et al.Geological-geo-chemical Prospecting Model of Large Precious Metal and Nonfer-rous Metal Deposits in China[M].Beijing:Geological Publishing House,2002,1～330.(in Chinese with English abstract).
[12]杨长春,刘兴材,李幼铭,等.地震叠前深度偏移方法流程及应用[J].地球物理学报,1996,39(3):409～415.Yang Changchun,Liu Xingcai,Li Youming,et al.A methodology for seismic prestack depth migration[J].Chinese Journal of Geo-physics,1996,39(3):409～415(in Chinese with English abstract).
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[14]陈光远,孙岱生,殷辉安.成因矿物学与找矿矿物学[M].重庆:重庆出版社,1987.1～780.Chen Guangyuan,Sun Daisheng,Yin Huian.Genetic Mineralogy and Prospecting Mineralogy[M].Chongqing:Chongqing Press,1987.1～780(in Chinese).
[15]赵玉琛.凹山玢岩铁流矿田的勘查历史和找矿预测[J].地质与勘探,1990,26(2):10～16.Zhao Yuchen.The Aoshan porphyrite Fe-S orefield:exploration history and prognostic exploration[J].Geology and Prospecting,1990,26(2):10～16(in Chinese with English abstract).
[16]蔡新平,刘秉光,季成云.滇西北衙金矿床特征及成因初探[J].黄金地质科技,1991,7:15～20.Cai Xinping,Liu Binguang,Ji Chenyun.Preliminary study on characteristics and genesis of Au deposit in Beiya area,west-ernYunnan Province[J].Gold Science and Technology,19917:15～20(in Chinese).
[17]蔡新平,刘秉光,季钟霖.金厂峪金矿的控矿构造及其地球物理验证[J].黄金科学技术,1994,2(5):1～7.Cai Xinping,Liu Bingguang,Ji Zhonglin.Ore-controlling structures of the Jinchangyu gold deposit and its geophysical validation[J].Gold Science and Technology,1994,2(5):1～7(in Chinese).
[18]赵永贵,王超凡,陈燕民,等.地震CT在寻找隐伏铜镍矿中的应用[J].地球物理学报,1996,39(2):272～278.Zhao Yonggui,Wang Chaofan,Chen Yanmin,et al.Seismic to-mography and its application to prospecting of concealed nickel-copper ore[J].Acta Geophysica Sicina,1996,39(2):272～278(in Chinese with English abstract).
[19]徐兴旺,蔡新平,梁光河,等.山东七宝山次火山杂岩区隐伏含矿角砾岩筒位-形-域精细预测[J].黄金科学技术,1999,7(2):9～18.Xu Xingwang,Cai Xinping,Liang Guanghe,et al.Detailed pre-diction on position,shape and size of concealed ore-bearing brec-cia pipes in the subvolcanic complex in Qibaoshan area,Shandong province[J].Gold Science and Technology,1999,7(2):9～18(in Chinese with English abstract).
[20]梁光河,蔡新平,张宝林,等.浅层地震勘探方法在金矿深部预测中的应用[J].地质与勘探,2001,37(6):29～33.Liang Guanghe,Cai Xinping,Zhang Baolin,et al.The application of seismic exploration method in deep prediction of gold deposits[J].Geology and Prospecting,2001,37(6):29～33(in Chinese with English abstract).
[21]梁光河,蔡新平,王杰,等.浅层地震勘探在云南北衙地区隐伏金矿预测中的应用[J].黄金科学技术,2000,8(6):1～9.Liang Guanghe,Cai Xinping,Wang Jie,et al.The application of seismic exploration method in prediction of concealed Beiya gold deposit in YunnanProvince[J].Gold Science and Technology,2000,8(6):1～9(in Chinese with English abstract).
[22]肖骑彬,蔡新平,徐兴旺,等.北京平谷盆地大地电磁测深勘查与隐伏含水岩溶系统的结构[J].吉林大学学报(地球科学版),2004,34(增刊):60～64.Xiao Qibin,Cai Xinping,Xu Xingwang,et al.Magnetotelluric sur-vey and structure of water-bearing karst system of Pinggu Basin,Beijing[J].Journal of Jiling University(Earth Science Edition),2004,34(增刊):60～64(in Chinese with English abstract).
[23]秦克章,方同辉,王书来,等.东天山板块构造分区、演化与成矿地质背景研究[J].新疆地质,2002,20(4):302～307.Qin Kezhang,Fang Tonghui,Wang Sulai,et al.Plate tectonics division,evolution and metallogenic settings in eastern Tianshan mountains,NW-China[J].Xinjiang Geology,2002,20(4):302～308(in Chinese with English abstract).
[24]Xu X W,Ma T L.Reply to the comment by Wen-Bin Zhu et al.on“Characteristics and dynamic origin of the large-scale Jiaoluo-tage ductile compressional zone in the eastern Tianshan Mountains,China”[J].Journal of Structural Geology,2004,26:2337～2340.
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