The thermal history of equilibrated ordinary chondrites and the relationship between textural maturity and temperature

Author:

Kessel Ronit,Beckett John R.,Stolper Edward M.

Publisher

Elsevier BV

Subject

Geochemistry and Petrology

Reference162 articles.

1. Regolith and megaregolith formation of H-chondrites: thermal constraints on the parent body;Akridge;Icarus,1998

2. QUILF—a PASCAL program to assess equilibria among Fe–Mg–Mn–Ti oxides, pyroxenes, olivine, and quartz;Andersen;Computers and Geosciences,1993

3. Armstrong J. T. (1988) Quantitative analysis of silicate and oxide materials: comparison of Monte Carlo, ZAF, and ϕ(ρZ) procedures. In: MicroBeam Analysis (ed. D.E. Newbury). San Francisco Press, Inc., San Francisco, pp. 239–246.

4. Algorithmic modifications extending MELTS to calculate subsolidus phase relations;Asimow;Am. Mineral.,1998

5. High pressure experimental calibration of the olivine–orthopyroxene–spinel oxygen geobarometer: implications for the oxidation state of the upper mantle;Ballhaus;Contrib. Mineral. Petrol.,1991

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