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Emplacement Mechanisms and Magmatic Differentiation Induced by Magma Flow in Sill Intrusions in Sedimentary Basins
(Doctoral thesis / Doktoravhandling, 2009)
Magma transport through the Earth’s crust often ends in sedimentary basins. While it erupts at the surface, a significant part of the magma emplaces in depth in the basin forming sheet complexes dominated by horizontal ...