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湖南水口山矿田与3号隐伏岩体有关的铁多金属矿床地质特征及找矿标志
引用本文:陈平波,刘继顺,宛克勇,徐卫娟,熊阜松,任远征.湖南水口山矿田与3号隐伏岩体有关的铁多金属矿床地质特征及找矿标志[J].矿产勘查,2016,7(3):450-455.
作者姓名:陈平波  刘继顺  宛克勇  徐卫娟  熊阜松  任远征
作者单位:中南大学地球科学与信息物理学院, 长沙 410000;湖南省有色地质勘查局二一七队, 衡阳 421000,中南大学地球科学与信息物理学院, 长沙 410000,湖南省有色地质勘查局二一七队, 衡阳 421000,湖南省有色地质勘查局二一七队, 衡阳 421000,湖南省有色地质勘查局二一七队, 衡阳 421000,湖南省有色地质勘查局二一七队, 衡阳 421000
基金项目:湖南省老矿山深部和外围找矿项目(编号:12120113083300)资助。
摘    要:在湖南常宁水口山矿田中部,新近发现了一个隐伏的夕卡岩型铁多金属矿床。该矿床产于3号隐伏花岗岩体接触变质交代蚀变破碎带中,受控于倒转背斜、花岗闪长岩体超覆体、栖霞组灰岩与当冲组砂页岩构成的接触带"三角地带",共伴生有铁、铜、铅、锌、银、金和铀。围岩蚀变组合复杂,其中石榴子石—透辉石—透闪石夕卡岩化、角岩化、硅化、大理岩化与成矿关系密切。矿床类型为接触交代成因的夕卡岩型。这一新类型矿体的发现,为水口山矿田隐伏矿体的找矿突破提供了新的方向与空间(隐伏岩体超覆体下接触变质交代带)。

关 键 词:水口山  铁多金属矿  地质特征  找矿标志  湖南
收稿时间:2015/8/10 0:00:00

Geological characteristics and prospecting criteria of skarn iron poly-metallic deposit related to No. 3 granite intrusion in the Shuikoushan ore field, Hunan
CHEN Ping-bo,LIU Ji-shun,WAN Ke-yong,XU Wei-juan,XIONG Fu-song and REN Yuan-zheng.Geological characteristics and prospecting criteria of skarn iron poly-metallic deposit related to No. 3 granite intrusion in the Shuikoushan ore field, Hunan[J].Mineral Exploration,2016,7(3):450-455.
Authors:CHEN Ping-bo  LIU Ji-shun  WAN Ke-yong  XU Wei-juan  XIONG Fu-song and REN Yuan-zheng
Affiliation:School of Geosciences and Info-Physics, Central South University, Changsha 410000;No.217 Team of Hunan Bureau of Geological & Exploration for Non-ferrous Metals Resources,Hengyang 421001,School of Geosciences and Info-Physics, Central South University, Changsha 410000,No.217 Team of Hunan Bureau of Geological & Exploration for Non-ferrous Metals Resources,Hengyang 421001,No.217 Team of Hunan Bureau of Geological & Exploration for Non-ferrous Metals Resources,Hengyang 421001,No.217 Team of Hunan Bureau of Geological & Exploration for Non-ferrous Metals Resources,Hengyang 421001 and No.217 Team of Hunan Bureau of Geological & Exploration for Non-ferrous Metals Resources,Hengyang 421001
Abstract:The skarn type iron poly-metallic deposit is discovered in central part of the well known Shuikoushan ore field recently. The orebody occurs in the contacted altered mineraliztion zone between No. 3 concealed granite intrusion and country rock. The orebody distribution is jointly controlled by overturned anticline, overlapping granodiorite intrusion, limestone of Qixia group and sandy shale of Dangchong group which formed a triangle structural zone. Main mineralization and associated elements are iron, copper, lead, zinc, silver, gold and uranium. The wall rock alteration varies is complex including garnet- diopside - tremolite skarn, hornfels, silicification and marbleization which are closely related to mineralization. The deposit type is contacted metasomatic skarn type. The discovery of new type orebody provides a clue for prospecting concealed orebody in the depth of Shuikoushan ore field, i.e., it is probably for finding new orebody in the contacted metamorphic zone under overlapping granite intrusion.
Keywords:Shuikoushan  skarn iron poly-metal deposit  geological characteristics  prospecting criteria  Hunan
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