Project Summary
Continents and sedimentary basins through time record fundamental Earth system cycles, reflecting environmental change, migration of fauna and flora and shifting coastlines. It was originally thought that successive advances and retreats of shallow inland seas mainly reflect global sea level variations (eustasy). It is now well known in principle that large-scale surface morphology such as the high topography of the East African Rift, the low-lying Amazon River Basin and the southwest to northeast tilt of the Australian continent are strongly controlled by processes deep within the Earth, but progress has been slow in quantifying the magnitude and time-dependence of these relationships. … Read more…
Tectonophysics – The Moho: boundary above upper mantle peridotites or lower crustal eclogites? A global review and new interpretations for passive margins
Mjelde, R., Goncharov, A., & Müller, R. D. (2013). The Moho: boundary above upper mantle peridotites or lower crustal eclogites? A global review and new interpretations for passive margins. Tectonophysics, 609, 636-650. doi: 10.1016/j.tecto.2012.03.001. The Moho: boundary above upper mantle peridotites or lower crustal eclogites? A global review and new interpretations for passive margins



