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上扬子台区下寒武统黑色岩系中的钒矿床
引用本文:鲍正襄,万榕江,包觉敏.上扬子台区下寒武统黑色岩系中的钒矿床[J].云南地质,2002,21(2):175-182.
作者姓名:鲍正襄  万榕江  包觉敏
作者单位:湘西地勘5队,湖南,乾洲,4160077
摘    要:我国南部早寒武世黑色岩系中,蕴藏丰富的金属和非金属矿产。而位于扬子地台东南缘的钒矿床尤其令人瞩目。本文以湘西为例,剖析该类钒矿地质特征和成矿规律。矿床产于下寒武统黑色岩系底产的碳系页岩、硅岩及黑色页岩组合。矿层呈层状、似层状,产权稳定,埋藏浅,储量大。矿石主要由水云母(伊利石)和石英组成,含有机质及藻类化石。成矿受地层、岩性、古构造和古地理条件控制。矿床具有微生物成矿与海底热水沉积双重特征,成因应属生物地球化学积积矿床范畴。

关 键 词:下寒武统  黑色岩系  钒矿床  地质特征  控矿因素  扬子地台  微生物  热水沉积
文章编号:1004-1885(2002)02-08
修稿时间:2001年7月3日

VANADIUM DEPOSITS OF BIACK SHAIE IN UPPER YANGTZE PLATFORM
BAO Zheng-xiang,WAN Rong-jang,BAO Jue-min.VANADIUM DEPOSITS OF BIACK SHAIE IN UPPER YANGTZE PLATFORM[J].Yunnan Geology,2002,21(2):175-182.
Authors:BAO Zheng-xiang  WAN Rong-jang  BAO Jue-min
Abstract:In South China,the Early Cambrian black rock series is rich in metallic and nonmetallic mineral ersources.And the V deposit in SE margin of the Yangzi platform is especially attractive. Taking the V deposit in west Hunan as an example,we analyse the geological characteristics and metallogenetic law of it.The ore deposit is occurred in the assemblage of carbonaceous shale,sillicalite and black shale of the bottom of Lower Cambrian black rock series.The ore beds are stratified,stratoid,with stable,shallow occurrence and large reserves.And the ore contains hydromica(illite),quartz,organic material and algal fossil.The metallogenesis ia controlled by strata,lithology,palaeostructure and palaeoggraphic conditions,characterized by microbial and seabed hydrothermal activities.The genesis of the ore deposit must belong to the biogeochemical sedimentation type.
Keywords:Vanadium Deposit  Geological Features  Ore-Controlling Factor  West Hunan
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