When continents break apart, continental crust and lithosphere are thinned until break-up is achieved and an oceanic basin is formed. The most remarkable and least understood structures associated with this process are up to 200 km wide areas of hyper-extended continental crust, which are partitioned between conjugate margins with pronounced asymmetry. Here we show, using high-resolution thermo-mechanical modelling, that hyper-extended crust and margin asymmetry are produced by steady state rift migration. … Read more…
Solid Earth – Plate tectonic raster reconstruction in GPlates
Cannon, J., Lau, E., & Müller, R. D. (2014). Plate tectonic raster reconstruction in GPlates. Solid Earth, 5(2), 741-755. doi: 10.5194/sed-5-741-2014. Plate tectonic raster reconstruction in GPlates



