Eustatic change modulates exhumation in the Japanese Alps

The exhumation of bedrock is controlled by the interplay between tectonics, surface processes, and climate. highest rates centimeters per year are recorded in zones highly active tectonic convergence such as Southern Alps New Zealand or Himalayan syntaxes, where high rock uplift combine with very processes. Using a combination different thermochronometric systems including trapped-charge thermochronometry, we show that also occur Hida Mountain Range, Japanese Alps. Our results imply centimeter more common than previously thought. thermochronometry data allow development time series rate changes at scale glacial-interglacial cycles, which four-fold increase baseline to ~10 mm/yr within past ~65 k.y. This likely explained knickpoint propagation due precipitation rates, climatic change, sea-level fall, range-front faulting, moderate uplift. resolve centimeter-scale sub-Quaternary changes, regions horizontal convergence, coupling climate, tectonics can exert significant rapid effect on exhumation.