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- W2391507472 abstract "The olivine xenocrysts,characterized by a deep source and produced by the disruption of the mantle peridotites,occur in the lamprophyre veins,which have close spatial temporal relationship with the gold vein,in the Dongshan ore block(-620~-670mlevel)and in the Xishan ore block(-50mlevel)of the Linglong gold deposit,Jiaodong peninsula.It is widely developed serpentinization and steatitization(serpentinization mainly in the Dongshan ore block and steatitization mainly in the Xishan ore block).According to alteration thermodynamics computations,the alteration temperature of Dongshan olivine xenocrysts was above 282℃ and was below 243℃ for Xishan olivine xenocrysts.On the basis of the above data,we concluded that the alteration temperature range of Dongshan olivine xenocrysts and Xishan olivine xenocrysts were 282~300℃ and 200~243℃,respectively.Our research provided new information for the Linglong deposit prospecting." @default.
- W2391507472 created "2016-06-24" @default.
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- W2391507472 date "2014-01-01" @default.
- W2391507472 modified "2023-09-23" @default.
- W2391507472 title "The Discovery of Olivine Xenocrysts of Lamprophyre in the Linglong Gold Deposit,Shandong and Its Prospecting Significance" @default.
- W2391507472 hasPublicationYear "2014" @default.
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