Metallogenic Regularity and Metallogenic Model of Vanadium Deposits in Xinglongchang Area,Luxi County,Hunan Province
Vanadium Deposits in Xinglongchang area occurred in the black rock series of the lower part of the Cambrian Niutitang Formation.The enrichment degree of vanadium deposits is closely related to the stratigraphic,lithofacies and tectonic.The formation of vanadium deposits is the result of the joint action of hot water deposition,normal seawater deposition and biogeochemical deposition.Based on the study of vanadium bearing rock series in the lower part of Niutitang Formation in Xinglongchang area,we have combined with field exploration and summarized the metallogenic regularity of Vanadium Deposits in this area.Based on the analysis of lithofacies paleogeography,the origin of vanadium deposit and the source of ore-forming materials,we are putting forward the metallogenic model of vanadium deposit.
Lower part of the Niutitang FormationVanadium bearing rock seriesMetallogenic regularityMetallogenic model
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