Geochemistry and oxygen isotope composition of main-group pallasites and olivine-rich clasts in mesosiderites: Implications for the “Great Dunite Shortage” and HED-mesosiderite connection

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Geochemistry and oxygen isotope composition of main-group pallasites and olivine-rich clasts in mesosiderites: Implications for the “Great Dunite Shortage” and HED-mesosiderite connection

Evidence from iron meteorites indicates that a large number of differentiated planetesimals formed early in Solar System history. These bodies should have had well-developed olivine-rich mantles and consequentially such materials ought to be abundant both as asteroids and meteorites, which they are not. To investigate this “Great Dunite Shortage” we have undertaken a geochemical and oxygen isot...

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New oxygen isotope evidence for the origin of mesosiderites and main group pallasites

Introduction: Many groups of differentiated achondrites display limited oxygen isotope variation, plotting within a restricted portion of the three-isotope diagram immediately below the terrestrial fractionation line [1,2]. As a consequence, oxygen isotopes have until recently been of only limited value in deciphering the relationships between these meteorite groups. A case in point is the appa...

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ژورنال

عنوان ژورنال: Geochimica et Cosmochimica Acta

سال: 2015

ISSN: 0016-7037

DOI: 10.1016/j.gca.2015.07.023