摘要
Shishugou deposits occur in the upper carboniferous Benxi group carbonate unconformity surfaces , and are strictly controlled by sedimentary discontinuous surfaces.The bauxite is large and stable ; Orebody is layered or lay-like structure ; Ore structure types are massive or layered structure ; The main mineral compositions are diasporite and kaolinite ; The harmful elements are less and associated with gallium elements , etc.Deposits by humid tropical climate change and formation of clay is closely related to mineralization , the different size depressions and dissolved buckets formed on the erosion surfaces are the positioning spaces of the bauxite ; The gulf lagoon deposition is favorable conditions for the bauxite bed formation.The deposits belong to main bauxite after short distance handling-machinery sedimentary , and have good bauxite metallogenic prospects.