The Mongol–Okhotsk Orogenic Belt is a major structural element in East Asia. Several aspects of its evolution remain unknown or controversial. In this study, we report the results obtained using 40Ar/
Raw LA-ICP-MS zircon and monazite data for samples from basement rocks of the Ries crater. The analytical method used, instrument set up, and data processing workflow are described in the published pa
This file contains the Geochronlogical data for granites and migmatites from the related study "Early Mesozoic anatexis-induced strain partitioning and gneiss doming in the Yunkai massif, South China:
Detrital K-feldspars and muscovites from Ocean Drilling Program Leg 116 cores that have depositional ages from 0 to 18 Ma have been dated by the 40Ar/39Ar technique. Four to...
