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Samples of zeolite ores collected from several deposits of the Muling zeolite orefield were analyzed by XRD, DTA, SEM, NAA, and EPMA. There is evidence that the migration of alkaline metal elements k and Na played an important role during zeolite mineralization. In forming of mordenite more Na+ might come in the mineralizing fluid and more K+ might come out of it, but in forming of clinoptilolite more K+ might come in the mineralizing fluid and more Na+ might come out of it. The formation of simple and mixed zeolie deposits might be related to the K-Na fractionation in the metallizing process: a higher K-Na fractionation is responsible for the formation of simple zeolite (mordenite or clinoptilolite) deposits, but a lower K-Na fractionation is responsible for the mixed zeolite (mordenite and clinoptilolite) deposits.
Samples of zeolite ores collected from several deposits of the Muling zeolite orefield were analyzed by XRD, DTA, SEM, NAA, and EPMA. There is evidence that the migration of alkaline metal elements k and Na played an important role during zeolite mineralization. of mordenite more Na + might come in the mineralizing fluid and more K + might come out of it, but in forming of clinoptilolite more K + might come in the mineralizing fluid and more Na + might come out of it. The formation of simple and mixed zeolie deposits might be related to the K-Na fractionation in the metallizing process: a higher K-Na fractionation is responsible for the formation of simple zeolite (mordenite or clinoptilolite) deposits, but a lower K-Na fractionation is responsible for the mixed zeolite (mordenite and clinoptilolite) deposits.