Fractional crystallization causes the iron isotope contrast between mid-ocean ridge basalts and abyssal peridotites
Open Access
- 25 March 2021
- journal article
- research article
- Published by Springer Science and Business Media LLC in Communications Earth & Environment
- Vol. 2 (1), 1-9
- https://doi.org/10.1038/s43247-021-00135-5
Abstract
No abstract availableFunding Information
- National Nature Science Foundation of China National Nature Science Foundation of China - Shandong Joint Fund for Marine Science Research Centers 111 Project
This publication has 62 references indexed in Scilit:
- The global pattern of trace-element distributions in ocean floor basaltsNature, 2012
- The oxidation state of Fe in MORB glasses and the oxygen fugacity of the upper mantleEarth and Planetary Science Letters, 2011
- Iron Isotopic Compositions of Geological Reference Materials and ChondritesGeostandards and Geoanalytical Research, 2010
- Iron isotopes may reveal the redox conditions of mantle melting from Archean to PresentEarth and Planetary Science Letters, 2009
- Origin of compositional trends in clinopyroxene of oceanic gabbros and gabbroic rocks: A case study using data from ODP Hole 735BJournal of Volcanology and Geothermal Research, 2009
- Nuclear resonant X-ray spectroscopy of (Mg,Fe)SiO3 orthoenstatitesEuropean Journal of Mineralogy, 2009
- Iron Isotope Fractionation During Magmatic Differentiation in Kilauea Iki Lava LakeScience, 2008
- Global Correlations of Ocean Ridge Basalt Chemistry with Axial Depth: a New PerspectiveJournal of Petrology, 2007
- Low degree melting under the Southwest Indian Ridge: the roles of mantle temperature, conductive cooling and wet meltingEarth and Planetary Science Letters, 2001
- Magmatic Oxides and Sulfides in Gabbroic Rocks from Hole 735B and the Later Development of the Liquid Line of DescentPublished by International Ocean Discovery Program (IODP) ,1991