Pre-eruptive storage conditions and continuous decompression relations of rhyodacite magma erupted from Chaos Crags, Lassen Volcanic Center, California

We performed a series of hydrothermal (high-temperature and -pressure) phase equilibrium experiments on a natural rhyodacite pumice from the 1103 ×13 years BP pyroclastic flow from the Chaos Crags, Lassen Volcanic Center, California. The pumice (LQ13-01, collected at the same location as LC84-417 (69.58 wt. % SiO2) by Clynne) is from the lower pyroclastic flow member of the group 1 lavas, the most silicic products known of Chaos Crags. Group 1 lavas are homogeneous (69-70 wt. % SiO2), petrographically and compositionally similar with rare to sparse mafic inclusions, and comprise the earliest emplaced units of Chaos Crags, the lower, middle, and upper pyroclastic flows, and domes A and B, whereas group 2 are comparatively heterogeneous (67-69 wt. % SiO2), with increasing abundance (10-15%) of mafic inclusions throughout the emplacement sequence, and comprise domes C through F. The phase assemblage in the natural sample used as experimental starting material comprises phenocrysts of quartz, plagioclase feldspars with rims of ~An35, biotite, hornblende, and Fe-Ti oxides in a vesiculated glassy matrix. Trace mafic enclaves are also present, but were removed from experimental starting material. All experiments were performed at the Smithsonian Institution. Experiments were run under H2O-saturated conditions at pressures of 75 MPa to 200 MPa and temperatures of 750°C to 900°C, at oxygen fugacity NNO+1 (×0.5-log-units), for 93 to 132 hours. EPMA and SEM analyses of experimental products show quartz is stable from <200 MPa at 750°C to <150 MPa at 800°C and is not stable at temperatures >800°C, within the investigated range. Amphibole is stable from >75 MPa at 750°C to >100 MPa at 800°C to 200 MPa at <850°C, and is not stable ≤75 MPa or ≥850°C. Biotite is stable at <800°C at 75 MPa to <825°C at 200 MPa, and not stable for any pressure at ≥850°C. Pyroxene, not present in the starting material is stable for 200MPa at >775°C and all pressures at temperatures ≥825°C, within the investigated range. FTIR analysis of quartz-hosted melt inclusions contain 4.0-5.0 wt. % H2O (average 4.3 wt. %), suggesting saturation pressures of 100-110 MPa (calculated using model of Papale et al., 2006). Comparison of the natural samples with the experimentally determined phase diagram and melt inclusions, suggests pre-eruptive storage conditions of 110-125 MPa and 775°C; given FeTi-oxide temperatures of 850 °C, magma may have been heated by as much as 75-100°C immediately prior to eruption. Ongoing work includes EPMA analysis of plagioclase feldspars and amphiboles to further constrain An-stability and hornblende-cummingtonite relations , respectively, and analysis of titanomagnetite-ilmenite pairs. Continuous decompression experiments are underway with rates ranging from 0.3 MPa/hr to 7.5 MPa/hr, corresponding to total decompression times of 16 hours to 18 days.