Abstract: Subridge Thermal Fluctuations Induced by Melting Low-Solidus Pyroxenite: Thermodynamic, Geochemical and Petrological Constraints (AGU Fall Meeting 2018)

Subridge Thermal Fluctuations Induced by Melting Low-Solidus Pyroxenite: Thermodynamic, Geochemical and Petrological Constraints

Daniele Brunelli^1,2, Enrico Bonatti^3,4, Marco Ligi³ and Anna Cipriani^5,6, (1)University of Modena and Reggio Emilia, Dipartimento di Scienze Chimiche e Geologiche, Modena, Italy, (2)Woods Hole Oceanographic Institution, Woods Hole, United States, (3)CNR Institute for Marine Science, Bologna, Italy, (4)Lamont Doherty Earth Observatory, Columbia University, Palisades, United States, (5)University of Modena and Reggio Emilia, Modena, Italy, (6)Lamont -Doherty Earth Observatory, Palisades, NY, United States

Back to: A Perfect Match: Bringing Together Models of Geodynamics and Thermodynamics to Understand Geochemical and Petrological Observations Posters