An Experimental Study of Trace Element Fluxes from Subducted Oceanic Crust
We have determined experimentally the hydrous phase relations and trace element partitioning behaviour of ocean floor basalt protoliths at pressures and temperatures (3 GPa, 750-1000°C) relevant to melting in subduction zones. To avoid potential complexities associated with trace element doping of s...
Main Authors: | , , , , |
---|---|
Language: | English |
Published: |
2017
|
Subjects: | |
Online Access: | http://doc.rero.ch/record/303317/files/egv046.pdf |