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Published byΣιλουανός Κασιδιάρης Modified over 6 years ago
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Bar diagram showing maximum length of sills in the various members in the study area.
Bar diagram showing maximum length of sills in the various members in the study area. The great length of sills in the regional mudstones, compared with the short maximum lengths attained in brittle homogeneous sandstone, and intermediate maximum lengths attained in brittle heteroliths and poorly cemented sandstone, should be noted. Christian Haug Eide et al. Journal of the Geological Society 2017;174:23-40 © 2017 The Author(s)
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