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fault breccia |
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fault breccia [′fȯlt ‚brech·ə] (geology) The assembly of angular fragments found frequently along faults. Also known as dislocation breccia. How to thank TFD for its existence? Tell a friend about us, add a link to this page, add the site to iGoogle, or visit webmaster's page for free fun content. |
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The stratigraphie levels of the host rock to each sampled fault breccia are shown on a lithological column (Fig. All but 4 of the Gold Summit holes intersected the McLean Pit fault breccia ("lode") extending, essentially uninterrupted by cross faulting, over 400 m along strike and 350m vertically with an average width of 15m. Previous records of the breccia have described it merely as a fault breccia (Dakyns et al. |
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