Pebbles of Neoproterozoic metaconglomerates of the Sedlčany-Krásná Hora metamorphic Islet were studied using geochemical and isotopic methods. The cadomian granitoid rocks were important source of these paraconglomerates.
Pebbles of Neoproterozoic metaconglomerates of the Sedlčany-Krásná Hora metamorphic Islet were studied using geochemical and isotopic methods. The cadomian granitoid rocks were important source of these paraconglomerates. (en)