Heinrich Bahlburg

The detrital zircon Hf and O isotope signals recorded in Paleozoic Saxothuringian clastic rocks of Germany: insights into the Eburnean and Cadomian orogenies

Saxothuringian sandstones of the Armorican Terrane Assemblage reflect a dichotomous detrital zircon age provenance signal representing the Eburnean Orogeny on the West African Craton (2200–2000 Ma) and the Cadomian Orogeny of northern Gondwana (750–540 Ma). We present O isotope d...