The reservoir characterization and provenance of the Wolfville Formation were investigated
using petrography, heavy minerals and microprobe analysis of tourmaline and garnet …

Abstract During Late Triassic time, the 357 m of Wolfville redbeds accumulated in a semiarid
rift valley near 20° N paleolatitude. Along the southern shore of Cobequid Bay, the formation …

Dolomitized coquinal facies of the Lower Triassic Montney Formation in western Alberta
(Fig. 1) contain close to 35× 10 6 m 3 (220 MM barrels) of initial volume in-place of crude oil …

The Devonian-Carboniferous Horton Group in the Man times Basin of Atlantic Canada was
deposited in local half grabens during an extensional phase that followed the Acadian …

The Fundy rift basin, comprising the contiguous Minas, Fundy, and Chignecto structural
subbasins (Figure 1), is filled by terrestrial redbed siliciclastics, minor carbonates, and …

Fundy Basin, one of a series of half graben that formed along the eastern margin of North
America during the Triassic/Jurassic rifting of Pangaea, lies mainly to the south of the …

The Lower Cretaceous fluvial sandstone–mudstone succession of the Chaswood Formation
is the proximal equivalent of offshore deltaic rocks of the Scotian Basin that are reservoirs for …

T he Orpheus graben is an eastward-plunging and widening fault-bounded subbasin of the
Scotian basin that shares a tectonic link with the nearby similar size Fundy rift basin. The …

The northern part of the Minas Sub-basin and the Cumberland Basin of northern Nova
Scotia and southeastern New Brunswick are adjacent to the Cobequid Highlands Massif …

Abstract The Swan Hills Formation at the Rosevear Field in Alberta, Canada is subdivided
into three major sedimentary packages (basal platform, platform reef, capping platform) that …