Reconstructing Plate Boundaries in the Jurassic Neo‐Tethys From the East and West Vardar Ophiolites (Greece and Serbia)
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DOI: 10.1002/2017tc004790
Abstract: Jurassic subduction initiation in the Neo-Tethys Ocean eventually led to the collision of the Adria-Africa and Eurasia continents and the formation of an ~6,000 km long Alpine orogen spanning from Iberia to Iran. Reconstructing the location… read more here.
Keywords: tethys; subduction; geometry; vardar ophiolites ... See more keywords