Exsolution lamellae in volcanic pyroxene; Single phenocryst thermometry for long-lived magmatic reservoir

Comprehensive understanding of the relevant timescales of thermal and chemical evolution of magma below the active volcanoes can help us to better anticipate volcanic eruptions and their likely precursor signals. In recent years, several lines of thermochronological inquiry have converged on a realization that, within many volcanic systems, magmas experience prolonged periods of relatively low-temperature storage prior to eruption during short duration transient events. This prolonged storage at low magmatic temperatures can result in series of solid state phase transformations within minerals, producing a petrologic record of their thermal history. In this example, we observed pigeonite exsolution lamellae in augite phenocrysts from the 2011 eruption of Cordon Caulle volcano, Chile. The small size of these features ( 70nm width and <1µm spacing), however, presents an analytical challenge. Focused ion beam (FIB) sample preparation has enable us to prepare site and orientation specific samples suitable for transmission electron microscope (TEM) characterization. Compositions of augite hosts (Wo39En38Fs22) were determined by EPMA prior to FIB preparation, while the compositions of pigeonite lamellae (Wo8En51Fs40) were determined by EDS utilizing PENEPMA simulation software for data reduction. These compositions yielded augite-pigeonite equilibrium temperatures of 945°C, in reasonable agreement with augite-liquid and bulk rock-liquidus temperatures. Lamella formation temperature relative to the C2/c → P21/c transition temperature can also be determined from the angle of the exsolution boundary with respect to crystal orientation. Since the C2/c → P21/c transition temperature is compositionally-dependent, however, calibration of this temperature-structure relationship requires us to conduct heating experiments. Toward this aim, we have combined nano beam electron diffraction (NBED) technique with an in-situ TEM heating stage to measure the changing lattice parameters at magmatic temperatures. Through this work we hope to develop two independent temperature determinations from individual augite phenocrysts which bear exsolution textures and apply this knowledge to understanding the thermal conditions of magma storage in long-lived volcanic reservoirs.