| 黄雷,周梵*.吉水县芦溪岭钼铜多金属矿床地质特征及找矿方向[J].南华大学学报(自然科学版),2012,26(4):36~42.[HUANG Lei,ZHOU Fan*.Prospecting and Geological Features of Molybdenum Copper Polymetallic Ore Deposit in Luxi Ridge，Jishui Country[J].Journal of University of South China(Science and Technology),2012,26(4):36~42.] |
| 吉水县芦溪岭钼铜多金属矿床地质特征及找矿方向 |
| Prospecting and Geological Features of Molybdenum Copper Polymetallic Ore Deposit in Luxi Ridge，Jishui Country |
| 投稿时间：2012-09-10 |
| DOI： |
| 中文关键词: 斑岩型钼（铜）矿 地质特征 矿床特征 找矿方向 |
| 英文关键词:porphyry molybdenum (copper) ore geological features deposit features prospecting direction |
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| 中文摘要: |
| 吉水县芦溪岭钼铜矿床属斑岩型矿床，矿床（体）受岩体内外接触带控制明显，裂隙带是控矿主要构造，也是矿化体的储矿构造.矿化体大致呈平行多层雁行式排列.矿石类型主要为花岗闪长斑岩型辉钼矿（黄铜矿）矿石、次为千枚岩型辉钼矿（黄铜矿）矿石.通过控矿因素分析，斑岩体内外接触带、断裂破碎带还具备寻找钼、铜、金、钨等矿床的潜力. |
| 英文摘要: |
| Molybdenum copper deposits of JiShuiXian LuXiLing belong to porphyry deposit.The ore body was obviously controlled by internal and external contact zone of rock mass.Fracture zone is accused of ore main structure,and is also the mineralized bodies mineral store structure.Mineralized bodies are roughly parallel layers of YanHang type arrangement.Ore type is mainly molybdenum (chalcopyrite) ore from granodiorite-porphyry,secondly is for molybdenum (chalcopyrite) ore from phyllite.Through the ore-controlling factors analysis,the internal and external contact zone and the fracture zone of porphyry still have the potential for looking for molybdenum,copper,gold,tungsten and other ore deposit. |
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