Experimental constraints on high pressure melting in subducted crust
Synthesis piston-cylinder experiments were carried out from 2.0 to 4.5 GPa and 850 to 1150°C in order to determine phase and melting relations in a model composition for subducted crust in H2O and large ion lithophile elements (LILE), this study concentr
|Collections||ANU Research Publications|
|Source:||Earth and Planetary Science Letters|
|01_Hermann_Experimental_constraints_on_2001.pdf||1.11 MB||Adobe PDF||Request a copy|
Items in Open Research are protected by copyright, with all rights reserved, unless otherwise indicated.