Abstract
The Late Proterozoic Bass River Complex of Nova Scotia, Canada, forms part of the Northern Appalachian Avalon terrane and comprises the Great Village River Gneiss, the platformal metasedimentary Gamble Brook Formation, and the mafic metavolcanic Folly River Formation. Three major periods of deformation within the complex are considered to be of late Precambrian age. The earliest (D1) appears to affect only the gneiss. The second additionally affects the Gamble Brook Formation and records polyphase ductile shear (D2a/D2b) along contacts with the gneiss attributed to sinistral transtension at c. 630 Ma. Locally sheeted, late-kinematic mafic dykes suggest limited crustal extension and may herald the development of basinal conditions in the Folly River Formation. The third deformation (D3a/D3b) records dextral transpression and polyphase, NW-directed thrusting in the Folly River Formation. D3 is tentatively attributed to basin closure during the latest Precambrian and may have accompanied thrust emplacement of late Precambrian bimodal volcanic rocks and turbidites preserved in the nearby Jeffers Group. Regional considerations suggest D2 and D3 kinematics respectively reflect the development and destruction of a late Precambrian volcanic arc rift.
- © The Geological Society 1990