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Central European Geology
Authors: Ildikó Gyollai, Ákos Kereszturi, Zsolt Kereszty, Máté Szabó, and Elias Chatzitheodoridis

split up to 2–3 sub-veins. The opaque minerals, mostly kamacite, occur along the walls of the shock veins. The chondrules in this zone are strongly fragmented (B6-1 and B5-1), and moved along the microfault in the shock veins. Between the shock veins

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