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Maunoir Ridge

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Journal Article
Published: 01 September 1992
Bulletin of Canadian Petroleum Geology (1992) 40 (3): 207–221.
... to range and within individual ranges. A number of Laramide structures, identifiable on seismic sections, have no surface expression, particularly to the north of Colville Hills (Fig. 6). A noteworthy example is the gas-bearing Tedji Lake anticline (Figs. 6, 8). Furthermore, Belot and Maunoir ridges plunge...
Journal Article
Published: 01 June 2011
Bulletin of Canadian Petroleum Geology (2011) 59 (2): 172–194.
... more subtle than those further south. The Aubry depocentre is a shallow feature located west of Aubry Lake. It is separated from the Horton depocentre by a NW trending low amplitude feature named Maunoir Ridge by Dixon and Stasiuk (1998) , who suggested that it might be related to a large scale...
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Journal Article
Published: 01 September 1998
Bulletin of Canadian Petroleum Geology (1998) 46 (3): 445–470.
..., with only two positive lements identified, of which only the most promi- nent is named (Maunoir Ridge, Fig. 3). There is an elongate gravity trend that appears to parallel the middle part of the Maunoir Ridge but for most of the thinning trend there is no obvious parallel trend in the gravity data (Fig. 4...
Journal Article
Published: 01 March 2020
Bulletin of Canadian Petroleum Geology (2020) 68 (1): 1–29.
...) interbedded with upper shoreface sandstone (F5). Given its location near Maunoir Ridge, and considering the interpreted depositional environments, the Mount Clark Formation in Stopover K-44 likely was deposited near the basin-margin, probably in a sheltered setting that was largely influenced by sea level...
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Journal Article
Published: 01 June 2014
Bulletin of Canadian Petroleum Geology (2014) 62 (2): 68–104.
..., unnamed ridge before terminating in Great Bear Plain. A central zone of thick Franklin Mountain Formation strata is evidence of enhanced Cambrian and Ordovician subsidence. The steep reverse fault must, therefore, once have defined the east boundary of an extensional graben ( Figs. 4B , 5B ). The western...
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Journal Article
Published: 01 June 1984
Bulletin of Canadian Petroleum Geology (1984) 32 (2): 139–146.
...’ and equivalents to north of 60°. One member of this family, the Leith Ridge fault, may have controlled a major offset in the latest Proterozoic continental margin. RÉSUMÉ Les données de forages profondes et d’affleurements indiquent la présence d’une structure précambrienne enfouie, orientée vers le Nord-Est et...
Journal Article
Published: 01 December 2016
Bulletin of Canadian Petroleum Geology (2016) 64 (4): 538–554.
... reserves in Canada’s North. During this time, Apache’s Lac Maunoir C-34 well was given an SDL based on recoverable oil, condensate, and gas reserves present ( Hannigan et al., 2011 ). Facies 3 is dominated by HCS, a high-energy sedimentary structure of oscillatory origin that records storm...
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Series: Memoir, Memoir
Published: 01 January 2012
DOI: 10.1306/13331661M983511
EISBN: 9781629810201
... ), and Mahony arch ( Pugh, 1993 ); in the north, Maunoir Ridge may be a Protero-zoic structure ( MacLean and Cook, 1992 ; Dixon and Stasiuk, 1998 ). The Mackenzie arch and Redstone arch ( Gabrielse, 1967 ; Gabrielse et al., 1973 ; Williams, 1987 ) are northwest-trending paleotopographic highs. The Mackenzie...
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