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High-grade contact metamorphism of calcareous rocks from the Oslo Rift, Southern Norway
High-grade metamorphism calcareous rocks Oslo Rift Southern Norway
2012/4/6
Shallow-levelplutonscausedextensivecontactmetamorphismofLowerPaleozoicshaleandcarbonatesequencesinthePermianOsloRift.A500mlongand100mwideshale-
limestonexenolithembeddedwithinmonzonitesbelongingtothe...