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Metamorphism of the Dalma Mafic Rocks
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The Precambrian Dalma metabasalts stretching for more than 200km represent original oceanic tholeiites. The metabasalts can be represented by eleven different groups of mineralogical assemblages ranging from low greenschist to high amphibolite facies. Spatial distribution of these six groups indicates increasing P-T conditions from east to west.
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