is located in the black rock series of South Qinling Mountains. It is a typical vanadium deposit controlled by the black rock series of Upper Ordovician Lower Silurian banjiuguan formation. Carbonaceous siliceous slate is the main ore bearing strata of the deposit
and the ore body is obviously controlled by strata. Based on the analysis of the ore controlling factors
enrichment rules
prospecting criteria and genesis of Huamiaozi vanadium deposit from the aspects of regional geology
deposit geology and ore body characteristics
it is considered that huamiaozi vanadium deposit is a shallow marine sedimentary layered deposit
belonging to syngenetic sedimentary gene
sis. The host strata are black rock series
such as carbonaceous siliceous rock
carbonaceous slate
carbonaceous mudstone
etc.
which are deposited in a shallow marine basin of the banjiuguan formation(O
3
-S
2
b).Carbonaceous siliceous slate(stone coal) is the main layer of vanadium ore body.