GARNET GEOCHRONOLOGY: IMPROVEMENTS AND APPLICATION IN HIMALAYAN RESEARCH (Invited Presentation)
In recent years, analytical advancements in selective garnet dissolution methods, chemical separation, and mass spectrometry have enabled high-precision garnet chronology (Lu-Hf, Sm-Nd) for increasingly smaller sample volumes. In addition, improved constraints on daughter-element diffusivity and empirical investigations into chronometric closure now enable robust age interpretation. At present, garnet chronology can be reliably done at precision levels of 0.5% or better with Lu-Hf and Sm-Nd methods, allowing precise age constraints on the timing, and even on the duration and progress, of garnet growth. When combined with modern P-T analysis, this approach yields supreme opportunities for investigating modern and ancient tectonics systems. In this contribution, we highlight some of the recent advances in garnet chronology and present newest findings from our garnet-based research in the High Himalaya and adjacent areas. Besides providing new insights into the tectonics of this complex Cenozoic mountain belt, the results yield new information on the duration of garnet growth in such systems, and the petro-chemical linkage between garnet and important chronometric minerals such zircon and monazite.