Mid-crustal deformation of the Annapurna-Dhaulagiri Himalaya, central Nepal: An atypical example of channel flow during the Himalayan orogeny

Parsons, A. J.Phillips, R. J.Lloyd, G. E.Law, R. D.Searle, M. P.Walshaw, R. D.2017-02-022017-02-022016-06-011553-040Xhttp://hdl.handle.net/10919/74905985 - 1015 (31) page(s)application/pdfenCreative Commons Attribution 4.0 InternationalGeosciences, MultidisciplinaryGeologyMAIN CENTRAL THRUSTINVERTED METAMORPHIC SEQUENCESOUTHERN TIBETSTRUCTURAL EVOLUTIONDUCTILE EXTRUSIONTECTONIC EVOLUTIONCONTINENTAL-CRUSTGREATER HIMALAYATHAKKHOLA GRABENLESSER HIMALAYAMid-crustal deformation of the Annapurna-Dhaulagiri Himalaya, central Nepal: An atypical example of channel flow during the Himalayan orogenyArticle - RefereedThe Author(s)Geospherehttps://doi.org/10.1130/GES01246.1123