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Pressure–temperature evolution of primordial solar system solids during impact-induced compaction

Author

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  • P. A. Bland

    (Curtin University)

  • G. S. Collins

    (Impacts & Astromaterials Research Centre (IARC), Imperial College London, South Kensington Campus, London SW7 2AZ, UK)

  • T. M. Davison

    (Impacts & Astromaterials Research Centre (IARC), Imperial College London, South Kensington Campus, London SW7 2AZ, UK)

  • N. M. Abreu

    (Earth Science Program, Pennsylvania State University—Du Bois Campus)

  • F. J. Ciesla

    (University of Chicago)

  • A. R. Muxworthy

    (Impacts & Astromaterials Research Centre (IARC), Imperial College London, South Kensington Campus, London SW7 2AZ, UK)

  • J. Moore

    (Impacts & Astromaterials Research Centre (IARC), Imperial College London, South Kensington Campus, London SW7 2AZ, UK)

Abstract

Prior to becoming chondritic meteorites, primordial solids were a poorly consolidated mix of mm-scale igneous inclusions (chondrules) and high-porosity sub-μm dust (matrix). We used high-resolution numerical simulations to track the effect of impact-induced compaction on these materials. Here we show that impact velocities as low as 1.5 km s−1 were capable of heating the matrix to >1,000 K, with pressure–temperature varying by >10 GPa and >1,000 K over ~100 μm. Chondrules were unaffected, acting as heat-sinks: matrix temperature excursions were brief. As impact-induced compaction was a primary and ubiquitous process, our new understanding of its effects requires that key aspects of the chondrite record be re-evaluated: palaeomagnetism, petrography and variability in shock level across meteorite groups. Our data suggest a lithification mechanism for meteorites, and provide a ‘speed limit’ constraint on major compressive impacts that is inconsistent with recent models of solar system orbital architecture that require an early, rapid phase of main-belt collisional evolution.

Suggested Citation

  • P. A. Bland & G. S. Collins & T. M. Davison & N. M. Abreu & F. J. Ciesla & A. R. Muxworthy & J. Moore, 2014. "Pressure–temperature evolution of primordial solar system solids during impact-induced compaction," Nature Communications, Nature, vol. 5(1), pages 1-13, December.
  • Handle: RePEc:nat:natcom:v:5:y:2014:i:1:d:10.1038_ncomms6451
    DOI: 10.1038/ncomms6451
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    Cited by:

    1. Kosuke Kurosawa & Gareth S. Collins & Thomas M. Davison & Takaya Okamoto & Ko Ishibashi & Takafumi Matsui, 2025. "Impact-driven oxidation of organics explains chondrite shock metamorphism dichotomy," Nature Communications, Nature, vol. 16(1), pages 1-8, December.

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