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河南省庙咀钒矿地质特征及成矿浅析
引用本文:张振生,胡呈祥,张文昭.河南省庙咀钒矿地质特征及成矿浅析[J].地质找矿论丛,2014,29(2):217-222.
作者姓名:张振生  胡呈祥  张文昭
作者单位:[1]河南省地质矿产勘查开发局第一地质勘查院,河南南阳473056; [2]河南美盛矿业投资有限公司,郑州450003; [3]中国地质大学(北京)能源学院,北京100083
摘    要:庙咀钒矿是近年查明的一个中型钒矿床。钒矿床地处荆紫关—师岗复向斜南翼,矿体赋存于下寒武统水沟口组底部硅质岩和泥岩中,严格受控于地层及岩性。矿石类型主要为黏土岩型及条带状硅质岩型两种,钒主要以离子吸附和类质同象赋存于黏土矿物中。矿床成因为滨海-浅海沉积型层控矿床。

关 键 词:庙咀钒矿  地质特征  矿床成因  找矿标志  河南省
收稿时间:2013/5/7 0:00:00

Geological feature and genesis of Miaozui vanadium deposit in Xichuan county, Henan province
ZHANG Zhensheng,HU Chengxiang and ZHANG Wenzhao.Geological feature and genesis of Miaozui vanadium deposit in Xichuan county, Henan province[J].Contributions to Geology and Mineral Resources Research,2014,29(2):217-222.
Authors:ZHANG Zhensheng  HU Chengxiang and ZHANG Wenzhao
Institution:ZHANG Zhensheng, HU Chengxiang, ZHANG Wenzhao (1. The First Geological Exploration Institute of Geological Exploration Bureau of Henan Province, Nanyang, 473056 Henan, China ; 2. Henan MeiSheng mining investment Co. L TD, Zhengzhou, 450003 China; College of Energy Resources, China University of Geosciences (Baijing) , Beijing, 100083,China)
Abstract:Miaozui is a medium vanadium deposit located in the south flank of Jingziguan to Shigang synclinorium of the South Qinling fold belt.Ore bodies occur in black siliceous rock and mudstone at bottom of Lower Cambrian Shuikougou Formation and are strictly controlled by strata and lithologies.Clay rock and banded siliceous rock are the two main ore types.Vanadium occurs mainly as absorbed ions and isomorphs in clay minerals.Genetically it is a littoral-shallow sea stratabound sedimentary V deposit.
Keywords:Miaozui vanadium deposit  geological feature  genesis  indicator for prospecting  Henan Province
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