López, S.Fernández Rodríguez, CarlosDonaire Romero, TeodosioCastro Dorado, Antonio2014-11-052014-11-052002http://hdl.handle.net/10272/9110The changes in the viscosity of bubble-bearing haplogranitic magmas with crystallinity are a prime function of the applied deformation rate. Under high deformation rates melt and magma viscosities are found to strongly increase with crystallinity. Low deformation rates promote, instead, a decrease in melt viscosity and a rather small increase in magma viscosity with crystallinity. These changes could explain some observed geological features in plutonsspaAtribución-NoComercial-SinDerivadas 3.0 Españahttp://creativecommons.org/licenses/by-nc-nd/3.0/es/Haplogranitic magmasBubblesViscosityRheologyjournal articleopen access