Magnetotelluric Study of the Hangai Dome, Mongolia: Phase II

Michael Becken, Alexey V. Kuvshinov, Matthew J. Comeau & Johannes Käufl
Surface deformation in the continental interior, away from active tectonic margins, is enigmatic, with the underlying mechanisms responsible not fully understood. Therefore, it is considered an open and important question in continental dynamics. The Hangai Dome, central Mongolia, is an ideal location to explore this because it is a high-elevation, low-relief, intra-continental region within the Mongolian plateau, between the Siberian and North China cratons, and within the Central Asian Orogenic Belt. The tectonic history of...
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