摘要
Intraplate processes,such as continental surface uplift and intraplate volcanism,are enigmatic and the underlying mechanisms responsible are not fully understood.Central Mongolia is an ideal natural laboratory for studying such processes because of its location in the continental interior far from tectonic plate boundaries.
基金
part of the research project"Crustmantle interactions beneath the Hangai Mountains in western Mongolia"
the financial support of the DFG and the SNF,awarded through the DACH program
