Fig. 18From: The Wechsel Gneiss Complex of Eastern Alps: an Ediacaran to Cambrian continental arc and its Early Proterozoic hinterlandPotential palaeogeographic relationships. The model for the suggested position of Wechsel arc is based on the recent proposal of Haas et al. (2020) (red star) with the major difference that a West African palaeogeographic relationship for the Cambrian is preferred (yellow star) (see text for discussion). Circles indicate the Late Archean/Early Proterozoic (Eburnean) crust and Late Ediacaran/Cambrian arc systems, which extend to South America (e.g., Ribeiro belt)Back to article page