Magma ascent in planetesimals: control by grain size

Magma ascent in planetesimals: control by grain size

Rocky planetesimals in the early solar system melted internally and evolved chemically due to radiogenic heating from 26Al. Here we quantify the parametric controls on magma genesis and transport using a coupled petrological and fluid mechanical model of reactive two-phase flow. We find the mean gra...

Полное описание

Библиографические подробности
Главные авторы:	Lichtenberg, T, Keller, T, Katz, R, Golabek, G, Gerya, T
Формат:	Journal article
Опубликовано:	Elsevier 2018

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