Evidence for the impact crater includes several examples of ‘shocked’ quartz grains in breccia (IMAGE)
Caption
Evidence for the impact crater includes several examples of ‘shocked’ quartz grains in breccia – a sedimentary rock type with large fragments cemented into a finer-grained matrix. The grains show signs of being deformed in the enormous pressures of the impact, which were between 10 and 30 gigapascals.
Credit
Sánchez-Garrido et al 2022.
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CC BY-NC-SA