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现代矿业 ›› 2017, Vol. 33 ›› Issue (10): 20-25.

• 地质·测量 • 上一篇    下一篇

粤北大宝山斑岩型钼矿床地质特征及找矿标志

潘会彬 曹艳超   

  1. 1.华北地质勘查局综合普查大队;2.黑龙江省有色金属地质勘查七一队
  • 出版日期:2017-10-25 发布日期:2017-10-25

Geological Characteristics and Prospecting Indicator of Dabaoshan Porphyry 〖JZ〗Molybdenum Deposit in Northern Guangdong Province

Pan HuiBin1Cao Yanchao2   

  1. 1.Exploration Unit of North China Geological Exploration Bureau; 2.The 701 Team,Heilongjiang 〖JZ〗Nonferrous Metals Geology Exploration Bureau
  • Online:2017-10-25 Published:2017-10-25

摘要: 大宝山斑岩型钼矿床是粤北地区典型的多金属矿床之一。结合该区地质工作成果,分析了矿区及矿床地质特征,进而系统总结了矿区找矿标志。研究表明:①矿区斑岩体由NNE向SW推覆并超覆于侏罗系地层之上,推覆体的主体即为钼矿体,区内矿化以钼为主,大体上具有浅部局部地段钨相对富集、深部钼相对富集的特征;②钼矿体产出于花岗闪长斑岩与寒武系碎屑岩、次英安斑岩的接触带,多呈似层状、透镜状,矿石类型以辉钼矿石为主,有少量辉钼矿黄铁矿矿石,主要金属矿物有辉钼矿和黄铁矿,钼矿化以不规则细脉、网脉状产出;③花岗闪长斑岩、次英安斑岩等燕山期中酸性浅成或超浅成侵入体以及硅化、绢英岩化等蚀变为矿区斑岩型钼矿床的重要找矿标志。在上述分析的基础上,进一步分析认为矿区主矿体(Ⅲ#钼矿体)产于斑岩体底部、推覆断裂构造面之上,与斑岩体的钾化、绢英岩化以及硅化关系密切,矿区已初步控制的矿体走向长大于600m,倾斜长大于650m,矿体自58#线往东和深部尚未有工程控制,因此,沿该矿体走向往东以及沿矿体倾斜方向宜进一步开展工作,有望扩大找矿前景。

关键词: 斑岩型钼矿,  地质特征,  找矿标志,  找矿前景

Abstract: Dabaoshan porphyry molybdenum deposit is one of the typical polymetallic deposits in Northern Guangdong Province.According to the geological prospecting and exploration results of the mining area,the geological characteristics of the mining area and the deposit are analyzed,and the prospecting indicators of the mining area are also summarized systematically.The study results show that:①Jurassic stratum is pushed and overlapped by porphyritic mass from NNE to SW in the mining area,the main body of the nappe rock mass is molybdenum orebody,the mineralization of the mining area is mainly for Mo,the local section of the shallow area of the mining area is rich for W,the depth of the mining area is rich for Mo;②the molybdenum orebodies are occurred in the contact zones of granodiorite porphyry and Cambrian clastic rock and dacite porphyry,they are distributed with the shapes of quasilamellar and lenticular,the ore type is mainly for molybdenite ore,and a small amount of pyritemolybdenite ore,molybdenite and pyrite are the main metal metallic minerals, the molybdenum mineralization is occurred with irregular veins and net veins;③Yanshanian mediumacid shallow or ultrashallow intrusions such as granodiorite porphyry and dacite porphyry and the silicification,sericitequartz alteration can be taken as the important prospecting indicators of the porphyry type molybdenum deposit in the mining area.Based on the above 〖CM42-104〗 study results,the further discussion results show that the main orebody (Ⅲ# molybdenum orebody) is 〖LM〗occurred in the bottom of porphyritic mass and the upper of the thrust fault structural surface,the main orebody is closely related to the potassium,sericite and silicification,the length of the orebody controlled in the mining area from the strike direction strike is more than 600 m,the length of the orebody controlled in the mining area from the tendency direction is more than 650 m,the east of 58# exploration line and the depth area are not controlled by exploration engineering,therefore,some prospecting and exploration works is necessary to be conducted along the east of the strike direction and tendency direction of the orebody,and the prospecting potential can be enlarged.

Key words: Molybdenum deposit, Geological characteristics, Prospecting indicator, Prospecting potential