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河南淅川李家湾钒矿床地质特征及成因初步研究
引用本文:吕文献,周世全,别建芳.河南淅川李家湾钒矿床地质特征及成因初步研究[J].矿产与地质,2010,24(3):235-240.
作者姓名:吕文献  周世全  别建芳
作者单位:1. 河南省地质调查院;河南省地勘局第一地质勘查院,河南,南阳,473500
2. 河南省地质调查院
摘    要:淅川李家湾钒矿处于扬子板块北缘,赋存于下寒武统水沟口组中下部。矿石类型为硅质岩型、页岩型及混合型三种。w(V2O5)一般在0.95%-1.34%。钒主要富集在下部硅质岩、上部杂色页岩,其中硅质岩与页岩互层者,以页岩为主,厚度大于硅质岩的组合内。钒的赋存状态呈高度富集和稀散分布两种。主要以离子吸附和类质同象赋存于粘土矿物中。与钙、钡呈正相关。矿床成因为陆棚相—浅海相层状沉积矿床。

关 键 词:钒矿床  矿床地质特征  矿床成因  找矿标志  李家湾  河南

Study on geological characteristics and genesis of vanadium deposit in Lijiawan, Xichuan country, Henan province
LV Wen-xian,ZHOU Shi-quan,BIE Jian-fang.Study on geological characteristics and genesis of vanadium deposit in Lijiawan, Xichuan country, Henan province[J].Mineral Resources and Geology,2010,24(3):235-240.
Authors:LV Wen-xian  ZHOU Shi-quan  BIE Jian-fang
Institution:1.Henan Institute of Geological Survey,Nanyang,Henan 473500;2.The First Geological Exploration Institute,Henan Provincial Bureau of Geo-exploration and Maineral Development,Nanyang,Henan 473500)
Abstract:The Lijiawan vanadium deposit of Xichuan country is located at the north rim of Yangzi plate,hosted in lower part of the lower Cambrian Shuigoukou formation.The type of the ore is siliceous rocks,shale or a mixture.V2O5 content is about 0.95-1.34%.Vanadium is rich in the bottom of the silicolite,upper of the variegated shale.In which the silicolite and the shale interbedding is mainly shale.The vanadium's mode of occurrence is highly rich or dispersion,which mainly occurred in the clay mineral by adsorption and isomorphism.It is positive correlation with calcium and barium.The contributing factor is continental shelf facies-shallow sea lamellar phase sedimentary ore deposit.
Keywords:vanadium deposit  geological characteristic of deposit  genesis of ore deposit  prospecting criteria  Lijiawan  Henan
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