Thick dyke emplacement and internal flow: A structural and magnetic fabric study of the deep‐seated dolerite dyke of Foum Zguid (southern Morocco)

Knowledge on forced magma injection and magma flow in dykes is crucial for the understanding of how magmas migrate through the crust to the Earth's surface. Because many questions still persist, we used the long, thick, and deep‐seated Foum Zguid dyke (Morocco) to investigate dyke emplacement and in... View More