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The Yanyuan region in the Emeishan large igneous province (ELIP) contains some low-Ti iron oxide deposits that are spatially associated with low-Ti basalts and related gabbroic intrusions. The Pingchuan deposit is the largest of this type and the adjacent Lanzhichang deposit is the first stratiform deposit hosted in the Emeishan basalts discovered in 2005. The Pingchuan deposit occurs in veins and...
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