Article ID Journal Published Year Pages File Type
4716357 Lithos 2012 20 Pages PDF
Abstract
► Wadi Ranga area form a belt of late Neoproterozoic volcanic-intrusive complexes. ► They formed through a transition from subduction related to intra-arc magmatism. ► Ranga volcanics are stratigraphically similar and tectonically different with Dokhan volcanics in north Arabian-Nubian Shield.
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Related Topics
Physical Sciences and Engineering Earth and Planetary Sciences Geochemistry and Petrology
Preview
Late Neoproterozoic volcanics and associated granitoids at Wadi Ranga, south Eastern Desert, Egypt: A transition from subduction related to intra-arc magmatism
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