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- W2366081811 abstract "There are many bedded skarns occurring as continuous beds are conformable with the wall rocks in which there are no zonings of typical contact metasomatism skarns.There are not characteristics of contact metasomatism skarn in the bedded skarn,which is mainly composed of garnet,diopsite,tremolite and chlorite.It's proved that the formation of the bedded skarn is not due to the contact metasomatism between the magmatic intrusion and the carbonate rocks,but the superimposed metasomatism in which the sedimentary rock or submarine volcanic sedimentary rock(basalt) of the Indo-Chinese epoch is reformed by the granitic intrusion of the Yanshanian epoch." @default.
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- W2366081811 date "2006-01-01" @default.
- W2366081811 modified "2023-09-25" @default.
- W2366081811 title "Research on Genesis of Bedded Skarn in Gejiu" @default.
- W2366081811 hasPublicationYear "2006" @default.
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