The Great Glen Crush Belt
نویسندگان
چکیده
منابع مشابه
Cenozoic reactivation of the Great Glen Fault , Scotland : Additional
13 The Great Glen Fault (GGF) trends NNE-SSW across northern Scotland. According to 14 previous studies, the GGF developed as a left-lateral strike slip fault during the Caledonian 15 Orogeny (Ordovician to Early Devonian). However, it then reactivated right-laterally in the 16 Tertiary. We discuss additional evidence for this later phase. At Eathie and Shandwick, minor 17 folds and faults in f...
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ژورنال
عنوان ژورنال: Geological Magazine
سال: 1953
ISSN: 0016-7568,1469-5081
DOI: 10.1017/s0016756800063901