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      Constraining central Neo-Tethys Ocean reconstructions with mantle convection models : MANTLE CONVECTION MODELS OF NEO-TETHYS

      , , , ,
      Geophysical Research Letters
      Wiley-Blackwell

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          Global continental and ocean basin reconstructions since 200Ma

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            India–Eurasia collision chronology has implications for crustal shortening and driving mechanism of plates

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              A plate tectonic model for the Paleozoic and Mesozoic constrained by dynamic plate boundaries and restored synthetic oceanic isochrons

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                Author and article information

                Journal
                Geophysical Research Letters
                Geophys. Res. Lett.
                Wiley-Blackwell
                00948276
                September 28 2016
                September 28 2016
                : 43
                : 18
                : 9595-9603
                Article
                10.1002/2016GL070524
                f0fe2839-e1bc-4293-a7f6-e1ffbe7a6b8b
                © 2016

                http://doi.wiley.com/10.1002/tdm_license_1.1

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