Microtextures in the Chelyabinsk impact breccia reveal the history of Phosphorus‐Olivine‐Assemblages in chondrites

Author:

Walton Craig R.1ORCID,Baziotis Ioannis2ORCID,Černok Ana3ORCID,Ferrière Ludovic4ORCID,Asimow Paul D.5ORCID,Shorttle Oliver16ORCID,Anand Mahesh37ORCID

Affiliation:

1. Department of Earth Sciences University of Cambridge Downing Street Cambridge CB2 3EQ UK

2. Department of Natural Resources Management and Agricultural Engineering Agricultural University of Athens IeraOdos 75 11855 Athens Greece

3. Department of Physical Sciences Open University Walton Hall Milton Keynes MK7 6AA UK

4. Natural History Museum Burgring 7 A‐1010 Vienna Austria

5. Division of Geological and Planetary Sciences California Institute of Technology 1200 E California Blvd Pasadena California 91125 USA

6. Institute of Astronomy University of Cambridge Madingley Road Cambridge CB3 OHA UK

7. Department of Earth Sciences The Natural History Museum London SW7 5BD UK

Funder

Science and Technology Facilities Council

Horizon 2020

Publisher

Wiley

Subject

Space and Planetary Science,Geophysics

Reference64 articles.

1. Phosphoran olivine from Pine Canyon, Piute Co., Utah

2. Chelyabinsk—Not only another ordinary LL5 chondrite, but a spectacular chondrite breccia (abstract #5171). 76th Annual Meeting of the Meteoritical Society.;Bischoff A.;Meteoritics & Planetary Science,2013

3. An experimental investigation into the metastable formation of phosphoran olivine and pyroxene

4. BoesenbergJ. S. EbelD. S. andHewinsR.2004.An experimental study of phosphoran olivine and its significance in main group pallasites (abstract #1201). 34th Lunar and Planetary Science Conference. CD‐ROM.

5. Pb–Pb dating constraints on the accretion and cooling history of chondrites

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