Explosive mantle-derived particles in sedimentary formations of the Carpathian region, connection with the problems of formation of fuels and ore deposits
Different types of mantle-derived particles were discovered in the Cretaceous-Paleogene sediments of the Carpathian region. Analogous mineral association has been found by previous investigations in the fluidized-explosive formations on the territory of Ukraine and other regions (Arkhangelsk, Yakutsk diamond province). Some data indicate that material is not redeposited and has a local origin. This suggests that at some stage have been favorable geodynamic conditions for the penetration of trans-mantle fluidized mixtures.