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- W2380099069 abstract "Shaerbuer Iron deposit was formed in a partial tension environment of an ancient arc zone. The orebodies have been found at the top of Silurian Shaerbuer group in layer, lens and moniliform characterized by multi stratum occurrence and massive, band and disseminated ore structure. There is jasper near orebodies and the deposit is characterized by under erosion. The total REE content in magnetite ore, minerals and red jasper is low with negative cerium and europium anomalies that are light REE enrichment characters. The decrepitation temperature of magnetite is high up to 370 430℃. The main ore fluid was magma water mixed with meteoric water.δ 30 Si in quartz of magnetite ore is close to that of jasper. Therefore it is proposed that the ore is origin in sea floor effusion and sedimentation." @default.
- W2380099069 created "2016-06-24" @default.
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- W2380099069 date "2002-01-01" @default.
- W2380099069 modified "2023-09-25" @default.
- W2380099069 title "GENESIS OF SHAERBUER SEA BOTTOM VALCANIC EFFUSIVE SEDIMENTARY MEGNETTE IN XINJIANG PROVINCE" @default.
- W2380099069 hasPublicationYear "2002" @default.
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