Curie Temperatures and Emplacement Conditions of Pyroclastic Deposits From Popocatépetl Volcano, Mexico

Abstract

Most pyroclastic deposits of Popocatépetl volcano were emplaced at high temperatures and have similar mafic to more evolved compositions, suggesting a long-lived, interconnected magma environment. We performed a magnetic and microscopic study on different eruptive sequences <14 ky in age and found that temperature and field dependence of magnetic susceptibility are suited to separate eruption phases. We observed homogeneous titanomagnetite with Curie temperatures (T$_{C}$) of 50–200°C and 200–400°C, together with different amounts of oxy-exsolved titanomagnetite with T$_{C}$ ∼ 570°C. Some block-and-ash flow deposits show remarkably irreversible T$_{C}$ in heating and cooling branches with a positive ΔT$_{C}$ (T$_{C}$ $_{heating}$ –T$_{C}$ $_{cooling}$) of up to 130°C in the center. The central part of this sequence is characterized by decreasing magnetic susceptibility and low field dependence of magnetic susceptibility (<10%), which is atypical for ulvöspinel-rich titanomagnetite. The nonreversibility of heating and cooling runs measured with rates of around 10 K/min is probably related to vacancy-enhanced nanoscale chemical clustering, which seems to occur preferentially during rapid quenching, possibly combined with subtle maghemitization. In contrast, pumice layers have the highest field dependence (∼20%) and contain Ti-rich and intermediate titanomagnetite with T$_{C}$ < 100 and ∼300°C, which are in line with mafic and more evolved magma composition. In intermediate phases, irreversibility of T$_{C}$ is more common but with a relatively low ΔT$_{C}$ of ±20°C. We suggest that magneto-mineralogy in pyroclastic density currents is complex but offers a complementary tool to the paleomagnetic directional analysis for emplacement temperature and contribute information on the volcanic material history and their emplacement conditions