Abstract: Impact-induced melting and heating of planetary interiors – implications for the thermo-chemical evolution of planets and crystallization of magma oceans (2017 AGU Fall Meeting)

Impact-induced melting and heating of planetary interiors – implications for the thermo-chemical evolution of planets and crystallization of magma oceans

Kai Wuennemann¹, Lukas Manske², Meng-Hua Zhu³, Miki Nakajima⁴, Doris Breuer⁵, Sabrina Schwinger⁵ and Ana-Catalina Plesa⁵, (1)Museum für Naturkunde Berlin, Berlin, Germany, (2)Museum für Naturkunde Berlin, Leibniz Institute for Evolution and Biodiversity Science, Berlin, Germany, (3)Macau University of Science and Technology, Taipa, China, (4)Carnegie Institution for Science, Department of Earth and Environmental Sciences, Washington, DC, United States, (5)German Aerospace Center (DLR), Institute of Planetary Research, Berlin, Germany

Back to: Accretion, Differentiation, and Early Planetary Evolution III