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Shock-induced kelyphite formation in the core of a complex impact crater

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Abstract

We present a compositional and textural analysis of shock-induced microtextures in garnet porphyroblasts in migmatitic garnet–cordierite–biotite paragneisses from the centre of the Vredefort impact structure, South Africa. Detailed imaging and major element analysis of deformation features in, and adjacent to, the garnet porphyroblasts record a complex, heterogeneous distribution of shock effects at the microscale. As the most competent silicate mineral in the assemblage, with the highest Hugoniot Elastic Limit and a wide pressure–temperature stability field, the porphyroblastic garnet preserves a more diverse shock deformation response compared to minerals such as quartz and feldspar, which underwent more comprehensive shock metamorphism and subsequent annealing. The garnet porphyroblasts display pre-impact fractures that are overprinted by later intra-granular Hertzian and distinctive planar fractures associated with the impact event. Shock-induced strain localization occurred along internal slip planes and defects, including pre-existing fractures and inclusion boundaries in the garnet. Symplectitic (kelyphitic) coronas commonly enclose the garnet porphyroblasts, and inhabit intra-granular fractures. The kelyphite assemblage in fractures with open communication beyond garnet grain boundaries is characterized by orthopyroxene—cordierite—sapphirine. Conversely, the kelyphite assemblage in closed-off intra-granular fractures is highly variable, comprising spatially restricted combinations of a secondary garnet phase with a majoritic component, Al-rich orthopyroxene, sapphirine and cordierite. The impedance contrast between garnet porphyroblasts and their inclusions further facilitated the formation of shock-induced features (Al-rich orthopyroxene coronas). Together, the textural and mineralogical data suggest that these features provide a record of oscillatory shock perturbations initiated under confining pressure beneath the transient crater floor. This occurred as the shocked rock volume underwent post-shock expansion, forming the core of the central uplift, and was followed by variable textural re-equilibration. This study thus provides a microtextural and mineralogical perspective of the shock regime within confined crust immediately prior to and during central uplift formation.

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Acknowledgements

Natalie Deseta’s Post-Doctoral Fellowship was supported by the Canadian Space Agency through a FAST program Grant awarded to JGS. Additional support came from grants awarded to JGS from the Natural Sciences and Engineering Research Council of Canada and the Canada Research Chairs program, as well as the South African NRF awarded to RG.

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Authors and Affiliations

  1. Planetary and Space Science Centre, University of New Brunswick, Fredericton, NB, E3B 5A3, Canada

    Natalie Deseta, Suporn Boonsue & John G. Spray

  2. School of Geosciences, University of the Witwatersrand (WITS), Private Bag 3, Johannesburg, 2050, South Africa

    Roger L. Gibson

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  1. Natalie Deseta
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  2. Suporn Boonsue
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Correspondence to Natalie Deseta.

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Communicated by Timothy L. Grove.

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Deseta, N., Boonsue, S., Gibson, R.L. et al. Shock-induced kelyphite formation in the core of a complex impact crater. Contrib Mineral Petrol 172, 84 (2017). https://doi.org/10.1007/s00410-017-1399-0

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