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Fig. 1 | Swiss Journal of Geosciences

Fig. 1

From: Fluid-driven low-grade metamorphism in polydeformed rocks of Avalonia (Arisaig Group, Nova Scotia, Canada)

Fig. 1

Map of the North Atlantic Borderlands in their pre-Mesozoic drift positions showing the distribution of Avalonia and other Neoproterozoic peri-Gondwanan terranes (modified from Strachan and Taylor 1990; Nance and Murphy 1994). The portion of Avalonia in Atlantic Canada is identified as West Avalonia, the portion in Britain and Ireland is known as East Avalonia. Only peri-Gondwanan terranes where Cambrian overstep sequences occur are identified (see Theokritoff 1979; Keppie 1985; Murphy et al. 2004; Landing 2005). AB Antigonish Basin, AH Antigonish Highlands, HF Hollow Fault, MB Maritimes Basin, MFZ Minas Fault Zone, SB Stellarton Basin

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