A Simple Thermodynamic Model for Melting of Peridotite in the System NCFMASOCr

• Published in: Journal of petrology Vol. 56; no. 5; pp. 869 - 892
• Main Authors: Jennings, Eleanor S., Holland, Tim J. B.
• Format: Journal Article
• Language: English
• Published: 01.05.2015
• Subjects: Liquids; Mantle; Mathematical models; Melting; Melts; Peridotite; Solidus; Thermodynamic models
• DOI: 10.1093/petrology/egv020
• ISSN: 0022-3530

A new thermodynamic model is presented for calculating phase relations in peridotite, from 0.001 to 60kbar and from 800 degree C to liquidus temperatures, in the system NCFMASOCr. This model system is large enough to simulate phase relations and melting of natural peridotite and basaltic liquids. Calculations in the program thermocalc illustrate mantle phase relationships and melting conditions, specifically for the peridotite composition KLB-1. The garnet-spinel transition zone intersects the solidus at 21.4-21.7kbar, where both Fe super(3+) and Cr increase spinel stability, expanding the width of the transition. Orthopyroxene is lost at the solidus at 42kbar in KLB-1, although this pressure is very sensitive to bulk composition. Calculated oxidation states are in excellent agreement with measured log fO sub(2) for xenolith suites with mantle Fe sub(2)O sub(3) contents in the range 0.1-0.3wt %. It appears that mantle oxidation state is not just a simple function of P and T, but depends on phase assemblage, and may vary in a complex way within a single assemblage. The liquid model performs well, such that calculated solidus, melt productivity and liquid compositions compare favourably with those of experimental studies, permitting its use in interpolating between, and extrapolating from, experimental P-T conditions. Experimentally challenging but geologically useful regimes can be explored, such as subsolidus samples and very low melt fractions, with application to both mantle xenoliths and the origin of basalt.