Petrogenesis of ungrouped enstatite meteorite Zakłodzie: Fabric, texture, and nanostructure analysis for identification of mechanisms responsible for chondrite–achondrite transition

1,2Agata M. Krzesińska,3Richard Wirth,3,4Monika A. Kusiak
Meteoritics & Planetary Science (in Press) Link to Article [https://doi.org/10.1111/maps.13296]
1Centre for Earth Evolution and Dynamics, Department of Geosciences, University of Oslo, Oslo, Norway
2Department of Earth Sciences, Natural History Museum, Cromwell Road, SW7 5BD London, UK
3GeoForschungsZentrum Potsdam, Section 3.5 Surface Geochemistry, D‐14473 Potsdam, Germany
4Institute of Geological Sciences Polish Academy of Sciences, ING PAN, Twarda 51/55, PL‐00818 Warszawa, Poland
Published by arrangement with John Wiley & Sons

Zakłodzie is an enstatite meteorite of unknown petrogenesis. Chemically, it resembles enstatite chondrites, but displays an achondrite‐like texture. Here we report on fabric and texture analyses of Zakłodzie utilizing X‐ray computed tomography and scanning electron microscopy and combine it with a nanostructural study of striated pyroxene by transmission electron microscopy. With this approach we identify mechanisms that led to formation of the texture and address the petrogenesis of the rock. Zakłodzie experienced a shock event in its early evolution while located at some depth inside a warm parent body. Shock‐related strain inverted pyroxene to the observed mixture of intercalated orthorhombic and monoclinic polymorphs. The heat that dissipated after the peak shock was added to primary, radiogenic‐derived heat and led to a prolonged thermal event. This caused local, equilibrium‐based partial melting of plagioclase and metal‐sulfide. Partial melting was followed by two‐stage cooling. The first phase of annealing (above 500 °C) allowed for crystallization of plagioclase and for textural equilibration of metal and sulfides with silicates. Below 500 °C, cooling was faster and more heterogeneous at cm scale, allowing retention of keilite and quenching of K‐rich feldspathic glass in some parts. Our study indicates that Zakłodzie is neither an impact melt rock nor a primitive achondrite, as suggested in former studies. An impact melt origin is excluded because enstatite in Zakłodzie was never completely melted and partial melting occurred during equilibrium‐based postshock conditions. Texturally, the rock represents a transition of chondrite and achondrite and was formed when early impact heat was added to internal radiogenic heat.

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