Spinel‐bearing, Al‐rich chondrules in two chondrite finds from Roosevelt County, New Mexico: Indicators of nebular and parent body processes

Abstract

Abstract— Two rare, spinel‐bearing, Al‐rich chondrules have been identified in new chondrite finds from Roosevelt County, New Mexico—RC 071 (L4) and RC 072 (L5). These chondrules have unusual mineralogies, dominated by highly and asymmetrically zoned, Al‐Cr‐rich spinels. Two alternatives exist to explain the origin of this zoning—fractional crystallization or metamorphism. It appears that fractional crystallization formed the zoning of the trivalent cations (Al, Cr) and caused a localized depletion in chromites around the large Al‐Cr‐rich spinels. The origin of the zoning of the divalent cations (Fe, Mg, Zn) is less certain. Diffusive exchange and partitioning of Fe and Mg between olivine and spinel during parent body metamorphism can explain the asymmetric zoning of these elements. Unfortunately, appropriate studies of natural and experimental systems to evaluate the formation of zoning of the divalent cations by fractional crystallization have not yet been conducted. The bulk compositions of the chondrules suggest affinities with the Na‐Al‐Cr‐rich chondrules, as would be expected from the abundance of Al‐Cr‐rich spinels. Melting of rare and unusual precursors produced the compositions of Na‐Al‐Cr‐rich chondrules, possibly including a spinel‐rich precursor enriched in Cr2O3 and ZnO. The two chondrules we studied have larger modal abundances of Al‐Cr‐rich spinels than reported in other Na‐Al‐Cr‐rich chondrules of similar composition, and Al‐rich chondrules even more enriched in spinel are reported in the literature. These differences indicate that factors other than bulk composition control the mineralogy of the chondrules. The most important of these factors are the temperature to which the molten chondrule was heated and the cooling rate during crystallization. These two chondrules cooled rapidly from near the liquidus, as indicated by the zoning, occurrence and sizes of spinels, radiating chondrule textures and localized chromite depletions. The range of mineralogies in other Al‐rich chondrules of similar composition reflect a range of peak temperatures and cooling rates. We see no reason to believe that this range is fundamentally different from the range of thermal histories experienced by “normal” Fe‐Mg‐rich chondrules.