粤北石—梅—师地区地球化学特征及钨矿远景预测
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摘要
粤北地区位于欧亚大陆板块与滨西太平洋板块消减带的内侧华夏板块的罗霄褶皱带,即武夷隆起西侧,罗霄褶皱带中部。属于南岭成矿带东段,是华南钨矿床最为富集的核心地带之一。
本文对粤北石-梅-师地区1:50 000水系沉积物测量和南山坑、穿风坳两矿点1:10 000土壤测量成果进行分析、研究,圈定了该地区W及与其相关成矿元素的1:50 000水系沉积物测量异常,结合野外实地调查、异常查证和矿点检查,初步总结了该区钨矿地球化学特征,在对区内典型钨矿成矿地质条件深入研究的基础上,对该区钨矿资源潜力进行了初步预测。
结合前人物、化探资料及国内典型钨矿床特征,认为区内巨大的东西向构造带和北东-北北东向断裂构造带是控制粤北石-梅-师地区矿床分布的主导构造因素,两个方向构造的结合部位是成矿最有利的区域。粤北石-梅-师地区主要有东西走向的良源-罗坝钨矿带、瑶-石-梅钨矿带和北北东走向的跃下-师姑山-杉木地钨矿带。
North Guangdong province is located in Luoxiao fold belt of the Cathaysian plate , inside the subduction zone between the Eurasian plate and western Pacific plate, namely the western of Wuyi uplift, the middle part of Luoxiao fold belt. The area is part of metallogenic zone of eastern nanling mountain, one of the center areas where have the most Tungsten deposits, south china.
The average of tungsten and its associated elements which come from the stream sediments of the area is extremely bigger than the area Clarke value. It indicates that tungsten and and its associated elements were enriched.The samples of stream sediments from Middle Cambrian strata, Lower and Middle Devonian strata, Upper and Middle Devonian strata and the third period of Early Yanshanian Granites.W, Mo, Bi have the strong relativity in the differents geological bodies, Mo and Bi are the best indicator elements for tungsten deposits.
There are twenty-one anomalies have been determined, they are ten second anomalies and eleven third anomalies.The anomalies of Tungsten and its associated elements form the huge E-W anomalous belts which from Wubanqiao to Xuantang and the N-N-E anomalous belts which from Yuexia to Shanmudi.The two anomalous belts intersect at the Nanshankeng Tungsten deposits, the biggest Synthetical Anomalies was formed at the area of Nanshankeng-Shibikeng-Yuzihu. Nanshankeng is the best Prospecting Target in the workaround.All the anomalous belts are controlled by sedimentary formation, magma's activities and Fault.
The 1﹕10 000 soil survey at Chuanfengao and Nanshankeng deposits are the check to the the stream sediments. The result of soil survey are mainly consistent, and the result has the very good guidable meaning.
The huge E-W tectonic and N-E,N-N-E faults belt are the main factors to control the distribution of Shi-Mei-Shi area, North Guangdong, the intersection of the two tectonics is the best area for a future Tungsten deposit.
The main mineralization types are quartz vein - fracture zones complex type, quartz vein- altered granite complex type, quartz vein type, skarn type and micro-disseminated type in lava five types.The Tungsten deposits of quartz vein - fracture zones complex type had been discovered a few years ago, as a new deposit type it being study now. The deposit exist in the fault system which is open comparatively. There isn’t strong relations between Yanshanian Granites and this type. The metallogenic temperature of this deposit type is lower than other types, most of them are middle-lower deposits, and been controlled by E-W faults obviously.
The analysis results of Geochemical and harvest of regional inventory and the inspect of deposits shows that there are three Tungsten Polymetallic Deposit belts ,they are E-W Liangyuan-Luoba Tungsten belt, E-W Yao-Shi-Mei Tungsten belt and N-N-E Yuexia-Shigushan-Shanmudi Tungsten belt.
本文对粤北石-梅-师地区1:50 000水系沉积物测量和南山坑、穿风坳两矿点1:10 000土壤测量成果进行分析、研究,圈定了该地区W及与其相关成矿元素的1:50 000水系沉积物测量异常,结合野外实地调查、异常查证和矿点检查,初步总结了该区钨矿地球化学特征,在对区内典型钨矿成矿地质条件深入研究的基础上,对该区钨矿资源潜力进行了初步预测。
结合前人物、化探资料及国内典型钨矿床特征,认为区内巨大的东西向构造带和北东-北北东向断裂构造带是控制粤北石-梅-师地区矿床分布的主导构造因素,两个方向构造的结合部位是成矿最有利的区域。粤北石-梅-师地区主要有东西走向的良源-罗坝钨矿带、瑶-石-梅钨矿带和北北东走向的跃下-师姑山-杉木地钨矿带。
North Guangdong province is located in Luoxiao fold belt of the Cathaysian plate , inside the subduction zone between the Eurasian plate and western Pacific plate, namely the western of Wuyi uplift, the middle part of Luoxiao fold belt. The area is part of metallogenic zone of eastern nanling mountain, one of the center areas where have the most Tungsten deposits, south china.
The average of tungsten and its associated elements which come from the stream sediments of the area is extremely bigger than the area Clarke value. It indicates that tungsten and and its associated elements were enriched.The samples of stream sediments from Middle Cambrian strata, Lower and Middle Devonian strata, Upper and Middle Devonian strata and the third period of Early Yanshanian Granites.W, Mo, Bi have the strong relativity in the differents geological bodies, Mo and Bi are the best indicator elements for tungsten deposits.
There are twenty-one anomalies have been determined, they are ten second anomalies and eleven third anomalies.The anomalies of Tungsten and its associated elements form the huge E-W anomalous belts which from Wubanqiao to Xuantang and the N-N-E anomalous belts which from Yuexia to Shanmudi.The two anomalous belts intersect at the Nanshankeng Tungsten deposits, the biggest Synthetical Anomalies was formed at the area of Nanshankeng-Shibikeng-Yuzihu. Nanshankeng is the best Prospecting Target in the workaround.All the anomalous belts are controlled by sedimentary formation, magma's activities and Fault.
The 1﹕10 000 soil survey at Chuanfengao and Nanshankeng deposits are the check to the the stream sediments. The result of soil survey are mainly consistent, and the result has the very good guidable meaning.
The huge E-W tectonic and N-E,N-N-E faults belt are the main factors to control the distribution of Shi-Mei-Shi area, North Guangdong, the intersection of the two tectonics is the best area for a future Tungsten deposit.
The main mineralization types are quartz vein - fracture zones complex type, quartz vein- altered granite complex type, quartz vein type, skarn type and micro-disseminated type in lava five types.The Tungsten deposits of quartz vein - fracture zones complex type had been discovered a few years ago, as a new deposit type it being study now. The deposit exist in the fault system which is open comparatively. There isn’t strong relations between Yanshanian Granites and this type. The metallogenic temperature of this deposit type is lower than other types, most of them are middle-lower deposits, and been controlled by E-W faults obviously.
The analysis results of Geochemical and harvest of regional inventory and the inspect of deposits shows that there are three Tungsten Polymetallic Deposit belts ,they are E-W Liangyuan-Luoba Tungsten belt, E-W Yao-Shi-Mei Tungsten belt and N-N-E Yuexia-Shigushan-Shanmudi Tungsten belt.
引文
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[2] 纪宏金,林瑞庆等.关于若干化探数据处理方法的讨论[J].地质与勘探,2001,37(4):56-59.
[3] 陈媚.辛金春化探背景与异常识刖的问题与对策[J].地质与勘探,1999,(2):25-29.
[4] 纪宏金,仲祟学.区域化探中若干新图件的计算与制作[J].物探化探计算技术,1991,(2):96-104.
[5] 纪宏金,连长云等.地球化学数据的标准化与衬度变换[J].物探化探计算技术,1993,(1):19-25.
[6] 陈永清,纪宏金.标准化区域地球化学图的编制方法及应用效果[J].长春地质学院学报,1995,(2):216-221.
[7] 吴轩,龚庆杰等.南岭地区区域化探数据中钨矿信息提取的方法探讨[J].物化探计算技术,2006,28(2):182-186.
[8] 阮天健,朱有光.地球化学找矿[M].北京:地质出版社,1990.
[9] 周柏生,张国华等.湖南瑶岗仙矿床化探异常特征及找矿前景[J].物探与化探,2002,26(6):436.
[10] 童潜明,伍任和等.郴桂地区钨、锡、铅、锌、金、银矿床成矿规律[M].北京:地质出版社,1995.
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[12] 刘卫明,钟盛文.大吉山钨矿床成矿的新认识[J].矿产与地质,1996,10(56):406-411.
[13] 赵妙琴.华南脉钨矿床中黑钨矿石英脉形成时成矿热液的对流循环运动[J].有色金属矿产与勘查,1998,7(5):272-277.
[14] 蒋国豪,胡瑞忠等.江西大吉山钨矿成矿年代学研究[J].矿物学报, 2004,24(3):253-256.
[15] 李大新,赵一鸣.江西焦里夕卡岩银铅锌钨矿床的矿化夕卡岩分带和流体演化[J].地质论评,2004,50(1):16-24.
[16] 张祖林,石荣求.江西有色地质勘查局钨矿勘查 50 年回顾[J].中粤北石-梅-师地区地球化学特征及钨矿远景预测 国钨业,1999,14(5-6):68-70.
[17] 刘家远.西华山钨矿的花岗岩组成及与成矿的关系[J].地质找矿论丛,2005,20(1)1-7.
[18] 周济元,肖惠良.成矿结构体系及其钨矿找矿意义[J].资源调查与环境,2006,27(2):110-119.
[19] 徐敏林,冯卫东等.崇义淘锡坑钨矿成矿地质特征[J].资源调查与环境,2006,27(2):159-163.
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