V53B-4845:
Geochemical-Seismological Imaging of Volatile-Assisted Melting at the Southern Margin of the Colorado Plateau, USA

Friday, 19 December 2014
Sean Rudzitis1, Mary R Reid1, Janne Blichert-Toft2 and Alan Levander3, (1)Northern Arizona University, Flagstaff, AZ, United States, (2)Ecole Normale Supérieure Lyon, Laboratoire de Géologie de Lyon, Lyon, France, (3)Rice University, Earth Science Department, Houston, TX, United States
Abstract:
Pliocene-Quaternary basalt-dominated volcanic rocks of the San Francisco-Morman Mountain fields (SFMM) erupted at the southern margin of the Colorado Plateau (CP) of the USA, a region of high continental elevation. The volcanic field is aerially extensive (>8,500 km2), and the youngest portion is located above the depth where the lithosphere-asthenosphere boundary (LAB) shoals to ~70 km. The volcanic fields also lie above and inboard of a band of low Vsthat encircles more than half of CP at <80 to 150 km depth. We obtained comprehensive new geochemical data for magnesian basalts (9-13 wt.% MgO) in order to better understand mantle melting associated with foundering of continental mantle lithosphere.

Melting of peridotite-dominated domains rather than lithologies that might have been introduced into the mantle by Laramide-aged shallow subduction are indicated by major element and transition metal signatures. The influence of subduction may nevertheless be recorded by moderately enriched isotopic compositions (εNd = -1.5 to +4.2; εHf= +5.5 to +11.8) that diverge from the mantle array. Trace element characteristics indicate variable mixtures of small degree melts (≤1%) generated in the garnet-stability field and melts generated at spinel stability conditions ± melt-rock reaction at the latter conditions.

Thermobarometry results for clinopyroxene-bearing SFMM basalts indicate magmatic temperatures of 1250-1330°C at or just below the Moho. Melting conditions delimited from olivine-melt equilibra mostly range from ~90 km to just above the seismic proxy for the LAB. More deeply equilibrated melts appear to have greater contributions from asthenosphere-derived melts, and melt contributions may by hybridized by localized convective upwelling in response to LAB migration. Melt equilibration temperatures are 80-130°C higher than for clinopyroxene crystallization, assuming that melts have water contents (~0.5 wt.%) inferred from mantle xenoliths. This could be reconciled by melting/melt reaction involving a more hydrous CP mantle, capable of producing melts with ~3 wt.% water, potentially the remnant of Laramide-aged flat-slab subduction.

This project is supported by NSF EarthScope Grant EAR-1109826.