江西南城蔡田金矿成矿规律研究
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摘要
文章以江西南城蔡田金矿普查为契机,按照"由表及里,由浅入深,由已知向未知"的原则寻找金矿,综合采用物化探、槽探(坑探)、钻探等方法,采集、分析样品,研究金矿的成矿规律。通过物化探手段,圈定F1'、F2'和F3'共3条断裂构造带,JD1～JD5共5条激电异常带,Ⅰ～Ⅶ共7个异常区域;通过槽探(坑探)、钻探等方法验证,圈出V1～V6共6条金矿(化)带;进一步研究金矿赋存规律,发现蔡田金矿符合浅成低温热液型特征。
Taking Caitian Gold Deposit of Nancheng, Jiangxi Province as an example, this paper in accordance with the principle of "from the beginning to the bottom, from the shallow to the deep, from the known to the unknown" to lookfor golddeposit. This paper comprehensive use of geophysical prospecting, trenching(pitting), drilling and other methods, collect and analyze samples,study the metallogenic regularity of Caitian gold deposit.By the means of geophysical exploration, We Circles theFl',F2'and F3' of three fault tectonic belts,JD1 ～ JD5 a total of 5 IP anomalybelts, Ⅰ～ Ⅶ of seven abnormal areas.Through the method of trenching(pitting),drilling and other methods,a total of 6 gold deposits were obtained from V1 ～ V6.Further studies on the occurrence regularity of gold mineralization shows that the CaitianGold Deposit is in accordance with the law of low-temperature hydrothermal type.
Taking Caitian Gold Deposit of Nancheng, Jiangxi Province as an example, this paper in accordance with the principle of "from the beginning to the bottom, from the shallow to the deep, from the known to the unknown" to lookfor golddeposit. This paper comprehensive use of geophysical prospecting, trenching(pitting), drilling and other methods, collect and analyze samples,study the metallogenic regularity of Caitian gold deposit.By the means of geophysical exploration, We Circles theFl',F2'and F3' of three fault tectonic belts,JD1 ～ JD5 a total of 5 IP anomalybelts, Ⅰ～ Ⅶ of seven abnormal areas.Through the method of trenching(pitting),drilling and other methods,a total of 6 gold deposits were obtained from V1 ～ V6.Further studies on the occurrence regularity of gold mineralization shows that the CaitianGold Deposit is in accordance with the law of low-temperature hydrothermal type.
引文
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庞奖励.1995.浅成低温热液矿床研究现状及进展[J],黄金地质,1(3),34~38.
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鄢云飞,谭俊,李闫华等.2007.中国浅成低温热液型金矿床地质特征及研究现状[J],资源环境与工程,21(1),7~11.
李碧乐,张晗.2010.浅成低温热液型金矿床研究的某些进展[J],矿物学报,30(1),90~97.
沙德铭,苑丽华.2003.浅成低温热液型金矿床特点、分布和找矿前景[J],地质与资源,12(2),115~124.
毛光武,曹亮,严卸平等.2015.浅成低温热液型金矿研究综述[J],地质找矿论丛,30(1),121~132.
刘一,骆学全,张雪辉等.2016.钦杭Cu-Au-Pb-Zn-W成矿带(东段)主要地质成矿特征及潜力分析[J],地质学报,90(7),1551~1572.
杨子江.2010.江西有色地勘局金矿勘查及金矿床研究回顾[J],矿产与地质,15(1),516-520.
黄爱玲.1998.江西省金矿类型及成矿特征[J],江西地质,12(2),129-132.
彭银生.2008.江西华南造山带东部金成矿的特征、成矿过程及前景分析[J],老区建设,31-32.
尹灵强、林建勇、陆振裕等.2017.江西省南城县蔡田金矿普查地质报告[R],江苏省核工业二七二地质大队,5.
王可勇,梁毓鎏,卢作祥.1999.江西金山金矿床地质特征及矿床成因探讨[J],地质与勘探,35(2),17-20.
吕文广,郑景宜,吕英平.1998.江西金山矿田金的赋存状态研究[J],矿产与地质,12(6),400-403.
徐华斌,苏朝晖,王明文.2013.江西金山金矿床地质特征及找矿方向[J],有色冶金设计与研究,34(1),1-3.
余金标.2001.东乡虎形山金矿地质特征[J],江西地质,15(4),267-270.
毛大华.1998.江西蛤蟆石金矿床地质特征及成因初探[J],江西地质,12(2),116-122.
程启开.2003.江西省银峰尖金矿床地质特征与找矿标志[J],矿产与地质,17(1),429-432.
李传明和陈小惠.2005.江西石坞金矿床成矿特征及找矿方向[J],地质与勘探,41(4),10-17.
钱姣风,许静.1998.江西茅排金矿床地质特征及找矿方向[J],江西地质,12(1),36-41.
彭银生.2008.茅排金矿床金矿化特征及成矿地质条件分析[J],铜业工程,11~14.
胡大千、姚杰.2007.江西茅排金矿矿物学找矿标志[J],世界地质,26(3),282~286.
张群喜.2007.江西临川茅排金矿韧-性剪切带特征及其金成矿动力机制探讨[J],黄金科学技术,15(5), 1~7.
《矿产资源工业要求手册》编委会.2010.矿产资源工业要求手册[M],地质出版社,203-210.
庞奖励.1995.浅成低温热液矿床研究现状及进展[J],黄金地质,1(3),34~38.
胡朋,赫英,张义等.2004.浅成低温热液金矿床研究进展[J],黄金地质,10(1),48~54.
鄢云飞,谭俊,李闫华等.2007.中国浅成低温热液型金矿床地质特征及研究现状[J],资源环境与工程,21(1),7~11.
李碧乐,张晗.2010.浅成低温热液型金矿床研究的某些进展[J],矿物学报,30(1),90~97.
沙德铭,苑丽华.2003.浅成低温热液型金矿床特点、分布和找矿前景[J],地质与资源,12(2),115~124.
毛光武,曹亮,严卸平等.2015.浅成低温热液型金矿研究综述[J],地质找矿论丛,30(1),121~132.