Spontaneous reheating of crystallizing lava

نویسندگان

چکیده

Abstract We show that recalescence, or spontaneous reheating of a cooling material due to rapid release latent heat, can occur during disequilibrium crystallization depolymerized Mg-rich melts. This only happen at fast rates, where the melt becomes undercooled by tens hundreds degrees before begins. Using forward-looking infrared (FLIR) camera, we documented recalescence in pyroxene (Fe, Mg)SiO3 and komatiite lavas initially cooled 25–50 °C s–1. Local heating front exceeds 150 for 10 lasts several seconds as migrates through. determined heat differential scanning calorimetry be 440 J g–1 275 with brief power output ∼100 W ∼300 MW m–3. Recalescence may widespread process solar system, particularly lava fountains, histories mafic pyroclasts should not assumed priori monotonic.

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ژورنال

عنوان ژورنال: Geology

سال: 2021

ISSN: ['0091-7613', '1943-2682']

DOI: https://doi.org/10.1130/g49148.1