Observations from ultrahigh-pressure metamorphic rocks combined with experimentally determined phase relations provide a framework for understanding fluid-mediated mass transfer in deeply subducted continental crust. At temperatures below 650 °C, aqueous
No takes yet. Share an insight, caveat, or question.
Hermann et al. (2013) studied this question.
Synapse has enriched 2 closely related papers on similar clinical questions. Consider them for comparative context: