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1 edition of The lower Paleozoic Misty Creek Embayment, Selwyn Basin, Yukon and Northwest Territories found in the catalog.

The lower Paleozoic Misty Creek Embayment, Selwyn Basin, Yukon and Northwest Territories

The lower Paleozoic Misty Creek Embayment, Selwyn Basin, Yukon and Northwest Territories

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Published by Dept. of Energy, Mines and Resources in Ottawa .
Written in English

    Subjects:
  • Geology - Yukon Territory

  • Edition Notes

    11

    The Physical Object
    Pagination78 p.
    Number of Pages78
    ID Numbers
    Open LibraryOL22007408M

    Northwest Territories (1) Yukon lower Paleozoic (Arenig) graptolite faunas in the Richardson Trough and Misty Creek Embayment, Yukon Territory and District of Mackenzie, Canada. Journal: Canadian Journal of Earth Sciences. Publisher. A foreland basin is a structural basin that develops adjacent and parallel to a mountain nd basins form because the immense mass created by crustal thickening associated with the evolution of a mountain belt causes the lithosphere to bend, by a process known as lithospheric width and depth of the foreland basin is determined by the flexural . Lower Paleozoic strata of the Cassiar terrane comprise part of a linear paleogeographic feature named the Cassiar platform (CP in Fig. 1B, Gabrielse, ; Fritz et al., ) or Pelly high (Cecile and Norford, ) that was located to the west of inboard elements such as the Selwyn basin, Kechika trough, and MacDonald by: 2. Assessing Undiscovered Resources of the Barnett-Paleozoic Total Petroleum System, Bend Arch–Fort Worth Basin Province, Texas * By. Richard M. Pollastro 1, Ronald J. Hill 1, Daniel M. Jarvie 2, and Mitchell E. Henry 1 Search and Discovery Article # ().


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The lower Paleozoic Misty Creek Embayment, Selwyn Basin, Yukon and Northwest Territories Download PDF EPUB FB2

PDF | On Jan 1,Michael P Cecile and others published Cecile, M.P. The Lower Paleozoic Misty The lower Paleozoic Misty Creek Embayment Embayment, Selwyn Basin, Yukon and Northwest Territories; Geological Survey of Canada. Cecile, M.P.

The Lower Paleozoic Misty Creek Embayment, Selwyn Basin, Yukon and Northwest Territories; Geological Survey of Canada Bulletin78 p.

Cecile, M.P. Geology of northeastern Niddery Lake map-area, Selwyn Basin Yukon and adjacent Northwest Territories; Geological Survey of Canada Bulletinp. bulletin the lower paleozoic misty creek embayment, selwyn basin, yukon and northwest territories m.p. cecile paleontologic appendix w.h.

fritz, b.s. norford af\id r.s. tipf\iis. oped passive margin in the early Paleozoic. The Misty Creek embayment, a northeastern extension of the deep-water lower Paleozoic Selwyn Basin, is immediately east The lower Paleozoic Misty Creek Embayment the Northwest Territories–Yukon border, and opens to the southwest into the Selwyn Basin (Fig.

First described by Cecile (), the geology of the Misty Creek embayment. Get this from a library. Selwyn Basin lower Paleozoic Misty Creek Embayment: Selwyn Basin, Yukon and Northwest Territories.

[M P Cecile]. The lower part of the Early Cambrian Sekwi Formation in the Selwyn Basin of the Northwest Territories, Canada, is composed of two regional, unconformity-bounded. Misty Creek Embayment, Yukon and Northwest Territories (Marmot Formation) Cecile, M.P.,The lower Paleozoic Misty Creek Embayment, Selwyn Basin, Yukon and Northwest Territories: Geological Survey of Canada, Bulletin78 p.

Selwyn basin, central Yukon (Menzie Creek formation). Add tags for "Lower paleozoic misty creek embayment, selwyn basin, yukon and northwest territories.". Be the first. The lower Paleozoic Misty Creek embayment, Selwyn Basin, Yukon and Northwest Territories; Geological Survey of Canada, Bulletin78 p.

Re-definition and subdivision of the Rapitan Group. The Selwyn Basin is a passive continental rift that underwent episodic extension and associated subsidence throughout the lower Paleozoic.

Alkalic volcanism, and spatially and temporally associated Ba and base metal mineralization, is concentrated along rift-parallel normal faults, particularly where these faults are offset by transform by: Biostratigraphical and ecostratigraphical significance of Tremadoc (Ordovician) graptolite faunas from the The lower Paleozoic Misty Creek Embayment Creek Embayment and Selwyn Basin in Yukon and Northwest Territories.

are also known from the Misty Creek Embayment in south- ern Y ukon and Northwest Territories (Jackson and Norford ), the Kechika Basin in northeastern British Columbia. Biostratigraphical and ecostratigraphical significance of Tremadoc (Ordovician) graptolite faunas from the Misty Creek Embayment and Selwyn Basin in Yukon and Northwest Territories D E Jackson, B S NorfordCited by: In the Ogilvie Mountains of west-central Yukon, intrusive breccias and volcanic rocks are aligned along faults that were active during evolution of the Cordilleran miogeocline.

Cecile, M. P.,The Lower Palaeozoic Misty Creek Embayment, Selwyn Basin, Yukon and Northwest Territories: Geological Survey The lower Paleozoic Misty Creek Embayment Canada Bulletin, no.

78 p Cited by: 8. Pages in category "Paleozoic life of the Northwest Territories" The following pages are in this category, out of total. This list Selwyn Basin not reflect recent changes (). Lithostratigraphy of deep-water lower Paleozoic strata in the central Misty Creek Embayment, Mackenzie Mountains, Northwest Territories.

GSC Current Research25 p. Hahn, K. and Selwyn Basin, E.C., Northwest Territories Geological Survey of Canada Publications relating to the Northwest Territories Yukon and Northwest Territories book. / THE LOWER PALEOZOIC MISTY CREEK EMBAYMENT, SELWYN BASIN, YUKON AND NORTHWEST TERRITORIES, Ottawa,pb, 78 pages, 44 figs.

(1 in pocket), 1 table, - 2 - $ Lithostratigraphy of deep-water lower Paleozoic strata in the central Misty Creek Embayment, Mackenzie Mountains, Northwest Territories. GSC Current Research25 p. Hahn, K. and Turner, E.C., Deep-water carbonate mound lithofacies, Borden Basin (Mesoproterozoic; NU).

Geological Survey of Canada, Current Research, v14 p. In the Selwyn Basin (Canada, Fig. 1) there are multiple occurrences of sediment-hosted barite (Cecile et al.,Goodfellow and Jonasson, ).Barite is a feature of Late Devonian shale-hosted massive sulphide (SHMS) mineralisation at MacMillan Pass District, Yukon (Ansdell et al.,Gardner and Hutcheon, ), and in the Gataga District, British Columbia (Paradis et Cited by: 5.

Neoproterozoic to Cretaceous age strata in the Mackenzie Mountains of the northern Canadian Cordillera record many geological events that affected the western margin of Ancestral North America. Two of these events that are the focus of this study are; (1) the development of a thick long-lived passive margin sequence of sedimentary rocks; and (2) continental rifting of this Cited by: The western continental margin is particularly well exposed and has been extensively studied in four main areas (), for which the stratigraphy is summarized in Fig.

2:(1) The Great Basin, which includes most of Nevada, and extends from the eastern limit of the Basin-and-Range tectonic province, the Wasatch Line, east of Salt Lake City, Utah, to the eastern margins of the Sierra Author: Andrew D.

Miall. Abstract. Taking the hydrocarbon source rocks of Ordovician, Lower Paleozoic in the Ordos Basin as the main research object, the characteristics of petroleum geological dynamics about geohistory, geothermal history, hydrocarbon generation history and hydrocarbon expulsion history were studied by using the methods of basin numerical modeling dynamically and pool-forming Cited by: 2.

Near the Howards Pass deposit in central Selwyn Basin (Fig. 1), this transition takes place in the Ordovician, while in the Misty Creek Embayment to the north, it occurred as early as Lower Cambrian.

atigraphy within the Selwyn Basin comprises chert and shale of the Road River Group, and shale and coarser clastics of the overlying Earn Group Cited by: The Bear River dykes (– Ma): westward continuation of the Mackenzie dyke swarm into Yukon, Canada.

The Tweed Lake basalts in the western Northwest Territories The lower Paleozoic Misty Creek Embayment, Selwyn Basin, Yukon and Northwest Territories.

Geological Survey of Canada, Bulletin78 pp. Google by: The book commences with a brief explanation of the assembly of Gondwana at the end of the Proterozoic and an overview of the distribution and structure of the onshore depocentres.

Four main phases of Paleozoic basin development are described: Cambrian intracratonic sag followed by three rift phases of Ordovician – Early Devonian, Middle.

west of the Yukon-Alaska border (6l°25’N, °70’W). Distal deposits of ash occur as primary airfall over much of Alaska, Yukon, and Northwest Territories. Locally resedimented deposits of ash are common closer to the volcanic source and occur in highly glaciated Size: 7MB.

Selwyn Basin, lying close to the Laurentia margin in Northwest Territories, has a well-known lower Paleozoic stratigraphy (e.g., Cecile, ; Cecile et al., ), with predominantly fine siliciclastics and minor by: 1. The Howards Pass district is in the Selwyn Mountains astride the Yukon-Northwest Territories border and consists at present of 15 distinct Zn-Pb deposits, containing Mt of ore with grades of 5 per cent Zn and 2 per cent Pb, that occur along the ‘zinc corridor’ (Selwyn Resource Ltd.

).Cited by: 8. Cover: Angular unconformity between Lower Paleozoic dolostone and Lower Proterozoic dolostone, near confl uence of Bond Creek and Wind River, 10 km west of study area, Wernecke Mountains (view to the southwest). Age difference across unconformity is at least billion years.

Yukon-Tanana BCBC Yukon Mtns. Ogilvie Mtns. Pelly Mtns. Cassiar Mtns. Wernecke Purcell Selkirk-Mtns. Rocky S. Canadian Mtns. trough Richardson platform Mackenzie embayment Misty Creek basin Selwyn platform MacDonald trough Kechika terrane Kootenay embayment Ospika trough Lardeau Mtns.

U.S. Rocky man line GSSZ d line yie er man line d line d. Base-metal enrichment in Stage-5 (mid-Cambrian) black shale of the Hess River Formation, Misty Creek Embayment (NT), Selwyn Basin; Turner, E C; in, Targeted Geoscience Initiative 4: Sediment-hosted Zn-Pb Deposits: processes and implications for exploration; Paradis, S (ed.).

Geologic History, Stratigraphy & Tectonics. The rocks of eastern Yukon, together with those in neighboring British Columbia and Northwest Territories formed beginning more than billion years ago in the region was at the western edge of the proto-North American continent Laurentia and in the uplifted mountains of the North American Cordillera, preserves.

M Compare and contrast the Lower Paleozoic evolution of the northern Cordilleran passive margin in Yukon and western Northwest Territories with that in the BC portion of the Cordillera, and explain these differences in terms of the development of upper and lower rifted plate boundaries and transfer faults such as the Liard Line.

Radiogenic and Stable Isotopic Compositions of mid-Cretaceous Intrusions in the Selwyn Basin, Yukon and Northwest Territories: Raven, Kenneth G.; Sean N. Sterling*, Richard E. Jackson, John D. Avis, Ian D. Clark: Geoscientific Site Characterization of the Proposed Deep Geologic Repository, Tiverton, Ontario.

Lower to Middle Paleozoic Petroleum Exploration Plays, Peel Plateau and Plain, Northern Mackenzie Corridor Mainland Sedimentary Basin in the Northwest Territories and Yukon, and is bordered to the south few Lower Paleozoic samples were collected, these indicate some gas-generating potential in.

A new Burgess Shale-type Lagerstätte is described from the middle Cambrian (Series 3, Drumian) Rockslide Formation of the Mackenzie Mountains, Northwest Territories, Canada. The Rockslide Formation is a unit of deeper water ramp to slope, mixed carbonate, and siliciclastic facies deposited on the northwestern margin of by: The Agate Basin Site book.

Read reviews from world’s largest community for readers. A Record Of The Paleoindian Occupation Of The Northwestern High Plains” as Want to Read: A Record Of The Paleoindian Occupation Of The Northwestern High Plains.

Write a review. Janice rated it it was amazing /5(5). 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.

The Lower Paleozoic Misty Creek Embayment, Selwyn Basin, Yukon and Northwest Territories. Geological Survey of Canada,GSC, Bulletin, Number 78 pages with 44 figures. Softbound, text and color geologic map in very good condition. $ Pages in category "Paleozoic life of Yukon" The following 80 pages are in this category, out of 80 total.

This list may not reflect recent changes (). The not so Passive Western Canadian Lower Paleozoic Cordilleran Margin pdf Plate Structure, Rift Basin (Misty Creek Embayment) Radiogenic and Stable Isotopic Compositions of mid-Cretaceous Intrusions in the Selwyn Basin, Yukon and Northwest Territories, Kirsten L.

Rasmussen, James K. Mortensen.download pdf, title = {Western Newfoundland, Canada, a lower paleozoic basin with hydrocarbon potential}, author = {Knight, I. and Hawkins, D.}, abstractNote = {Western Newfoundland hosts an early Paleozoic passive margin that was destroyed by later convergence and is now preserved in a foreland fold and thrust belt.

Autochthonous Cambrian-Ordovician .Paleozoic Petroleum Systems ebook the Canning Basin, Western Australia: A review* By.

K.A.R. Ghori 1 and P.W. Haines 1 Search and Discovery Article # () Posted February 3, *Adapted from extended abstract prepared for presentation at AAPG International Conference and Exhibition, Perth, Australia, November