• Continental crust was formed during metamorphic events in amalgamated supercontinents. Granites by dehydration melting (upper crust) and mantle-derived fluids (lower crust). Mantle reach the middle-upper along shear zones generate granites. Until middle of 20th century, continental considered to be dominantly granitic. This hypothesis revised after Second World War when several new studies le...

Major and trace element composition of silicate melt inclusions (SMI) their rock-forming minerals were studied in mafic garnet granulite xenoliths from the Bakony–Balaton Highland Volcanic Field (Western-Hungary). Primary SMIs occur clinopyroxene plagioclase plagioclase-rich domains granulites ilmenite vicinity these wall rock. Based on major elements, we demonstrated that have no connection wi...

Abstract This study presents the new petrology and geochemistry data for comprehension of origin emplacement conditions Lolodorf mafic rocks whitin Nyong Complex. The meta-mafic consist fine-grained garnet (FGM) coarse-grained (CGM) presenting nearly similar mineral composition. They are made up quartz, plagioclase, orthopyroxene, clinopyroxene, amphibole, opaques, apatite rutile. also present ...