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- W2392144471 abstract "Xiaorequanzi copper deposit occurred mainly in C 1x volcano-sedimentary rock associations with a normal sedimentary rock. The ore bodies are stratiform or stratoid in the depth and vein form at the shallows,displaying an overpass pattern mineralization.Detailed study on the basic geology, ore geology and geochemistry revealed that the formation of this deposit can be divided into 4 epochs and 6 stages, that is, exhalation-sedimentary epoch, superimposed-reform epoch of mixed hydrothermal solution,reform epoch by the structure process and weathering process. The second epoch is the most important mineralization epoch." @default.
- W2392144471 created "2016-06-24" @default.
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- W2392144471 date "2002-01-01" @default.
- W2392144471 modified "2023-09-25" @default.
- W2392144471 title "A STUDY ON ORE-FORMING PROCESS OF THE XIAOREQUANZI COPPER DEPOSIT, XINJIANG" @default.
- W2392144471 hasPublicationYear "2002" @default.
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