Bridgmanite Freezing in Shocked Meteorites Due To Amorphization?Induced Stress

نویسندگان

چکیده

Bridgmanite, the most abundant mineral in Earth's lower mantle, can be found meteorites that experienced instantaneous high shock pressure during parent body impact. However, presence of bridgmanite is unusual because grains should amorphized under residual post-shock temperatures at ambient pressure. Here, we report results time-resolved synchrotron X-ray diffraction measurements to analyze amorphization mechanisms and kinetics bridgmanite. The thermal expansion coefficient before 2.1 × 10?5 K?1. At higher temperatures, our show significant volume due induces static stress reach up ?0.5 GPa, which prevents progress amorphization. This time-insensitive may have enabled preservation shocked meteorite fell on Earth. Also, reaction estimated based amorphous fraction provides temperature.

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ژورنال

عنوان ژورنال: Geophysical Research Letters

سال: 2022

ISSN: ['1944-8007', '0094-8276']

DOI: https://doi.org/10.1029/2022gl098231