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- W2374100729 abstract "The Xuanlong type iron deposit is located in the Chenjiayao region,Chicheng County,Hebei Province.Influenced by the heating power from the Yanshanian intrusive granite in the depth and surrounding areas,the Xuanlong type hematite was metamorphosed into magnetite by the organic carbon in the host rock in the oxygen- lacking reducing condition.The siliceous dolomite and limestone of Tuanshanzi Formation on the top of Xuanlong type iron formation are partly metamorphosed into wollastonite and diopside.At the atmospheric pressure,the formation temperature of wollastonite is about 400℃,considering the Yanshanian granite shows the characteristics of plutonic rockmass,therefore it predicts that the temperature of hematite metamorphosed into magnetite is a range between 400 ℃ and 600 ℃." @default.
- W2374100729 created "2016-06-24" @default.
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- W2374100729 date "2013-01-01" @default.
- W2374100729 modified "2023-09-28" @default.
- W2374100729 title "Discussion on the genesis of Chenjiayao iron deposit,Hebei" @default.
- W2374100729 hasPublicationYear "2013" @default.
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