Abstract Deposition of the Sauk megasequence of northwestern Canada, from Peace River in British Columbia (north of lat. 56°N) to the Beaufort Sea in the Northwest Territories and Yukon Territory (lat. ∼70°N), occurred along a complex segment of the rifted western margin of Laurentia. This synthesis describes the stratigraphy, depositional history, tectonic setting, and resource potential associated with the development of the Cambrian-Ordovician great American carbonate bank. There have been few detailed studies of the Sauk megasequence in these remote areas of Canada, and much information on platform and equivalent facies remains at a reconnaissance scale. Platform rocks occur as relatively flat-lying strata of the Interior Platform that thin eastward onto the Canadian shield and correlate westward to strata within the deformed belt of the Canadian Cordillera. It is generally accepted that the Sauk megasequence was deposited along the subsiding rifted margin of Laurentia because facies pass from shallow-marine settings to deeper water slope and basinal settings from east to west. Abrupt facies changes, thickness changes, and intercalated volcanic rocks in most successions suggest a setting more complex than a simple passive margin during the development of the Cambrian-Ordovician great American carbonate bank. During Sauk megasequence deposition, positive and negative tectonic features controlled deposition along the continental margin and are represented by distinct present-day physiographic regions. The northern Rocky Mountains region lies between 56 and 60°N and is included in this summary because its geologic history is more similar to regions to the north, instead of to the southern Cordillera. North of 60°N latitude, five main regions span the vast northern Canadian mainland sedimentary basin: Beaufort-Mackenzie, Interior Plains, Mackenzie Arc, Northern Yukon, and Selwyn-Cordillera. The lower Paleozoic succession is poorly known in the “Beaufort-Mackenzie Basin,” a term that typically refers only to uppermost Cretaceous to Holocene Mackenzie Delta sediments. The northern Rocky Mountains region lies north of Peace-Athabasca arch. The arch was a positive area and forms the southern limit to the Macdonald platform and the Kechika trough, a graben system that flanked the platform to the west. The Kechika trough accumulated mainly shallow-water siliciclastic sediments until the Late Cambrian, and Sauk I and II super-sequences are characterized by complex facies changes. Carbonate deposition was prominent in the Middle Cambrian when bioherms developed on tilted fault blocks in the western part of the Kechika trough. The uppermost Cambrian–Ordovician Sauk III stratigraphy records deposition during postrift passive-margin thermal subsidence; however, during the middle Sauk III supersequence, a distinct east-to-west platform-to-basin setting evolved in response to renewed extension along the margin. The Interior Plains region lies mainly in the Northwest Territories and contains a subsurface record of the Mackenzie platform. In the Cambrian, the area was an epicontinental marine basin consisting of several depocenters that opened to the south and were segmented by positive high elements such as the Mackenzie arch. Lower and Middle Cambrian units are siliciclastic dominated and discontinuous because of the extent of paleogeographic highs. Extensive Sauk III platform carbonates of the Mackenzie platform were deposited beginning in the latest Cambrian. The Mackenzie Arc region is the eastern part of the foreland belt in Yukon and the Northwest Territories. It offers a more continuous stratigraphic record compared with the Interior Plains, but abrupt facies changes from north to south suggest phases of extension. The region contains deformed strata of the Mackenzie platform, the Mackenzie arch, and the eastern part of Selwyn Basin, which extended into the platform as Misty Creek embayment. The Sauk I supersequence is siliciclastic dominated, and carbonates are present only in distal slope settings. Sauk II and III supersequences are carbonate dominated, representing expansion of the Macdonald platform across the Mackenzie arch. Prominent slope facies in the Sauk II and III supersequences suggest an abrupt platform-to-basin setting that also accumulated submarine volcanics during phases of extension. The Selwyn-Cordilleran region extends from southwestern Yukon and northeastern British Columbia to the international border with Alaska. It is an area of deformed incompetent strata that were deposited in the Selwyn Basin, west of the Mackenzie Arc. The region contains autochthonous North American strata east of the Tintina Fault, and parautochthonous and al-lochthonous terranes west of the fault. One parautochthonous terrane thought to be a displaced slice of the North American margin is the Cassiar terrane or Cassiar platform. The Sauk mega-sequence of Selwyn Basin is generally similar to that of the Mackenzie Arc region, although the Sauk I and II supersequences contain additional units of distal basinal siliciclastic facies. The northern Yukon region contains several mountain belts and intermontane basins or lowlands that contain a succession with overall similarities to the North American Sauk mega-sequence, although the record is poorly understood in this remote area. The main tectonic element is a broad area of platform carbonates, the Yukon stable block, which is bordered to the east by the Richardson trough and to the south by the Selwyn Basin. The lower Sauk I supersequence is absent because of uplift of the Ogilvie arch. Block faulting influenced a mostly siliciclastic-dominated Sauk II supersequence, although deposition of carbonate resumed during deposition of the upper Sauk II supersequence and persisted throughout the Sauk III supersequence deposition. Sauk megasequence carbonates that may have been part of the great American carbonate bank underwent abrupt lateral facies changes indicative of syndepositional extension during the Early to Middle Cambrian, and again in the Middle Ordovician. These tectonic complexities, coupled with the lack of detailed studies, preclude a comprehensive sequence-stratigraphic analysis and determination of relative or eustatic sea level changes. The base of the Sauk megasequence is a prominent sub-Cambrian unconformity in most regions; however, eastward (toward the craton), this surface represents a merger of several unconformities, and westward (basinward), various Cambrian units overlie Proterozoic rocks. The base of the Tippecanoe megasequence, although muted and less clear in thicker shelf and offshelf successions, lies in the Middle or Upper Ordovician. The Sauk I supersequence is dominated by shallow-water siliciclastic deposits, many of which are localized in extent, with rare carbonate in distal settings such as the Selwyn Basin. Carbonate units of the middle to upper Sauk I supersequence were most likely deposited basinward of a carbonate platform. The best record of Sauk II carbonate deposition occurs along the margins of the Selwyn Basin or is represented bynarrow tracts associated with block faulting. The basal parts of the Sauk III supersequence are poorly known, but significant Upper Cambrian terrigenous siliciclastic rocks in some regions suggest a phase of uplift. The Sauk III supersequence is otherwise characterized by widespread deposition of carbonate platform and equivalent slope and basin deposits at the edge of platforms during widespread transgression and continued margin subsidence. The vast area of northwestern Canada has both hydrocarbon and mineral resource potential in rocks of the Sauk megasequence, although exploration is limited by remoteness and lack of infrastructure. Early Paleozoic intracratonic and platform-to-basin settings of the margin accumulated both potential source and reservoir rocks for fluid hydrocarbons. The Colville Hills area of the Interior Plains region has the most significant discovery of gas and some condensate within Cambrian strata. This basal Cambrian siliciclastic play potentially exists across the Interior Plains. Porous reservoir facies of Cambrian–Ordovician platform carbonates constitute another potential play, and abundant source rocks are present within equivalent basinal facies. Although mountainous regions have little hydrocarbon potential because of their geologic history, some Cambrian–Ordovician rocks host mineralized zones, particularly in the Selwyn-Cordillera region such as the metallogenic belt of Zn-Pb-Ag sedimentary exhalative deposits of the Anvil district along the western margin of the Selwyn Basin.

Abstract Sequences of Upper Proterozoic, dominantly clastic, sedimentary rocks, generally assigned to the Windermere Supergroup, are commonly more than 2000 m thick and are exposed almost continuously throughout the length of the eastern Cordillera (Fig. 6.1, 6.2). In the Purcell and Mackenzie mountains the supergroup unconformably overlies strata of the Purcell and Mackenzie Mountains supergroups, respectively. In and near the Omineca Belt the rocks unconformably overlie basement of granitic gneiss ranging in age from 728 Ma to more than 2 Ga (see Chapter 4). Elsewhere, the lower contact of the supergroup is not exposed. In many places the supergroup is overlain unconformably by clastic rocks, commonly sandstone, of Early Cambrian age, but in more western areas, whereLower Cambrian rocks may be fine grained, an unconformable relationship is difficult to demonstrate. Characteristically, in the central and southern Cordillera, the lower part of the Windermere Supergroup comprises thick, monotonous sequences of gritty, feldspathic sandstone, siltstone and shale, variably metamorphosed from low greenschist to upper amphibolite facies. The upper part of the Windermere is more calcareous and much more variable in lithology. One or more carbonate formations are of regional significance although correlationsbetween regions are dubious. Conspicuous maroon, purple and green shale occurs in the uppermost formation of the group in the Selwyn, northern Rocky, Cassiar, Omineca and Cariboo mountains. In the Selwyn Mountains the varicoloured shales overlie thick successions of gritty sandstone that are younger than most grits assigned to the Windermere Supergroup elsewhere. Diamictite, at least locally reflecting glacial

Abstract “Asbestos” is the general term applied to fibrous silicate minerals which are commercially valuable because they are resistant to heat and chemical attack and exhibit high tensile strength. Chrysotile is by far the most important asbestos mineral, accounting for more than 95% of consumption. The balance is made up by asbestiform varieties of amphibole, including riebeckite (variety crocidolite), cummingtonite (variety amosite), anthophyllite, tremolite, and actinolite. Almost all chrysotile is mined from vein deposits in serpentinized ultramafic rocks. A small amount is derived from either mass fibre deposits in serpentinitesor from serpentinized dolomites. This section deals only with deposits of chrysotile asbestos in serpentinized ultramafic rocks. The most important deposits in Canada include the Jeffrey mine at Asbestos, Quebec; the Bell-King-Beaver deposit at Thetford Mines, Quebec; the British Canadian and Black Lake mines at Black Lake, Quebec; the Asbestos Hill deposit in the Ungava region of Quebec; the Advocate mine at Baie Verte, Newfoundland; the Cassiar mine in British Columbia; and the Clinton Creek mine in Yukon Territory (Fig. 11-1). Important foreign deposits include Dzhetygara in Kazakhstan; Bazhenovo in Russia; Msauli in the Republic of South Africa; Havelock in Swaziland; Mang'ai in Qinghai, China; and Cana Brava in Goias, Brazil.

Abstract The Canadian Cordillera is a region of great geological and metallogenic diversity. Just as each Cordilleran terrane preserves a stratigraphic record different from those of neighbouring terranes, characteristic suites of mineral deposits, as integral parts of their host terranes, reflect fundamental differences in their depositional environments. The miogeocline and displaced equivalents in the eastern Cordillera, as well as each of the terranes comprising the accreted collage of the western Cordillera, possess unique lithotectonic characteristics that are reflected in the types of mineral deposits they contain. Predominantly stratiform deposits of Zn, Pb, Cu, Ba, and Fe and skarn deposits of W, Zn, Pb, Mo, and Sn are hosted by layered sedimentary strata of the ancestral North American miogeocline. The similar types of mineral deposits of displaced (Cassiar) and/or deformed (Kootenay, Nisling) continental margin terranes support their cratonal linkage. Stikinia and Quesnellia, which together constitute the bulk of the Intermontane Superterrane, host a suite of mineral deposits typical of their predominantly calc-alkalic volcanic-arc composition: abundant porphyry Cu,Mo deposits, Cu, Zn volcanogenic massive sulphides, Cu and Au skarns, and Au,Ag veins. On the other hand, the ophiolitic Cache Creek and Slide Mountain terranes of the Intermontane Superterrane display distinctive kinds of mineral deposits typical of their oceanic origin: magmatic Cu,Ni, volcanogenic Cu,Zn and mesothermal Au veins, in addition to ultramafic pluton-related asbestos, jade, Cr and platinum group element (PGE) deposits. The dominantly arc volcanic character of the diverse terranes of the Coast Belt is reflected in their metallogeny: volcanogenic Cu,Zn, porphyry Cu,Mo,