关键词: 热年代学, 碎屑颗粒, 盆-山耦合

Abstract:

The unreseted mineral grain with low closure temperature (such as zircon and aptite FT and felspar Ar-Ar dating system) located in clastic sedimentary sequence records much information about the process of mountain building and basin deposition. So it becomes a main object of detrital grain thermochronology. Detrital grain thermochronology is a promising method for recovery of basement exhumation history, for determining provenance and the maximum deposition age and for stratigraphic correlation. We first

Key words: Thermochronology, Detrital grain, Coupling between basin and mountain