Drupal-Bibcite0<style face="normal" font="default" size="100%">Detachment folding of partially molten crust in accretionary orogens: A new magma-enhanced vertical mass and heat transfer mechanism</style><style face="normal" font="default" size="100%">Detachment folding of partially molten crust in accretionary orogens: A new magma-enhanced vertical mass and heat transfer mechanism</style>