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The migmatitic lower plate of the Ruby Mountains–East Humboldt Range (RM–EHR) metamorphic core complex of northeastern Nevada represents a deep section of the hinterland of the Sevier orogenic belt. New major and trace element (Zr-in-rutile, Ti-in-biotite) thermobarometry is aided by garnet zoning analysis and a thermodynamic modeling approach involving melt reintegration. The P–T history for rock...

The P–T History of Anatectic Pelites of the Northern East Humboldt Range, Nevada: Evidence for Tectonic Loading, Decompression, and Anatexis