Search Results

You are looking at 1 - 1 of 1 items for :

  • Earth and Environmental Sciences x
  • Refine by Access: Content accessible to me x
Clear All
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

Open access