The extremely reduced silicate‐bearing iron meteorite Northwest Africa 6583: Implications on the variety of the impact melt rocks of the IAB‐complex parent body. (6th December 2013)

• Record Type: Journal Article
• Authors: Fazio, Agnese; D'Orazio, Massimo; Folco, Luigi; Gattacceca, Jérôme; Sonzogni, Corinne
• Is Part Of: Meteoritics & planetary science. Volume 48:Number 12(2013:Dec.)
• Page Start: 2451
• Page End: 2468
• Publication Date: 2013-12-06
• Subjects: Meteorites -- Periodicals; Planetology -- Periodicals; 523.4
• DOI: 10.1111/maps.12231
• Languages: English
• ISSNs: 1086-9379

Abstract

<abstract abstract-type="main" id="maps12231-abs-0001"> <title>Abstract</title> <p>Northwest Africa (NWA) 6583 is a silicate‐bearing iron meteorite with Ni = 18 wt%. The oxygen isotope composition of the silicates (∆′¹⁷O = −0.439 ‰) indicates a genetic link with the IAB‐complex. Other chemical, mineralogical, and textural features of NWA 6583 are consistent with classification as a new member of the IAB‐complex. However, some unique features, e.g., the low Au content (1.13 μg g⁻¹) and the extremely reducing conditions of formation (approximately −3.5 ∆IW), distinguish NWA 6583 from the known IAB‐complex irons and extend the properties of this group of meteorites. The chemical and textural features of NWA 6583 can be ascribed to a genesis by impact melting on a parent body of chondritic composition. This model is also consistent with one of the most recent models for the genesis of the IAB‐complex. Northwest Africa 6583 provides a further example of the wide lithological and mineralogical variety that impact melting could produce on the surface of a single asteroid, especially if characterized by an important compositional heterogeneity in space and time like a regolith.</p> </abstract>