New Paleomagnetic Data on Carboniferous-Permian Geological Complexes of Mongolia

摘要

One of the main problems of paleomagnetic studies is assessment of the displacement of geological blocks relative to cratons, because the marginal part of cratons is the site of formation of new continental crust forms and development of active volcanism. The width of oceans, as well as the position of island arcs, back-arc basins, and other geological structures, are established precisely with respect to cratons.