Corrigendum to “Sulfide in dunite channels reflects long-distance reactive migration of mid-ocean-ridge melts from mantle source to crust: A Re-Os isotopic perspective” (Earth and Planetary Science Letters (2020) 531, (S0012821X19306612), (10.1016/j.epsl.2019.115969))
State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan, 430074, China; ARC Centre of Excellence for Core to Crust Fluid Systems (CCFS), GEMOC, Department of Earth and Planetary Sciences, Macquarie UniversityNSW 2109, Australia; State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Beijing, 100083, China; Departamento de Mineralogía y Petrología, Facultad de Ciencias, Universidad de Granada, Avda. Fuentenueva s/n, Granada, 18002, Spain; Geosciences Montpellier, CNRS UMR5243, Université de Montpellier, Pl. E. Bataillon, Montpellier, 34095, France
Recommended Citation:
Xiong Q.,Xu Y.,González-Jiménez J.M.,et al. Corrigendum to “Sulfide in dunite channels reflects long-distance reactive migration of mid-ocean-ridge melts from mantle source to crust: A Re-Os isotopic perspective” (Earth and Planetary Science Letters (2020) 531, (S0012821X19306612), (10.1016/j.epsl.2019.115969))[J]. Earth and Planetary Science Letters,2020-01-01,535