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- W2386553467 abstract "The Quanling tremolite deposit is located in the southeastern part of the Panshi-Shuangyang fold cluster, which is occurred in the contact alteration zone of intermediate acidity magmatic rock and Shizuizi Formation carbonate sedimentary formation, and which belongs to skarn type deposit. From ore type, the tremolite is dominant, which mainly applies it to ceramic industry." @default.
- W2386553467 created "2016-06-24" @default.
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- W2386553467 date "2005-01-01" @default.
- W2386553467 modified "2023-09-25" @default.
- W2386553467 title "The deposit characteristics of the Quanling tremolite, Panshi area, and its developing prospect" @default.
- W2386553467 hasPublicationYear "2005" @default.
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