Summary Account of Mesozoic and Tertiary Stratigraphy, Canadian Arctic Archipelago.

by Geological Survey of Canada.

Publisher: s.n in S.l

Written in English
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Edition Notes

1

SeriesPaper (Geological Survey of Canada) -- 60-05
ContributionsTozer, E.T.
ID Numbers
Open LibraryOL21906086M

The book contains 45 extensively illustrated articles. It starts with papers on the Mesozoic source rocks, and oceanic natural gas clatrates in the Arctic, respectively. Then follow articles on the regional and petroleum geology of the main regions; Greenland, North American Arctic, Soviet Arctic and the Barents Sea. Since Tertiary sediments are considered much later than marine Paleozoic and Mesozoic sediments, advocates reason that the mammals must be the progeny of those animals that survived on the Ark, and thus, post-Flood. Tertiary mammals are found in the high intermountain basins in the western United States and in High Plains strata. MESOZOIC STRATIGRAPHY AT DURANGO, COLORADO SPENCER G. LUCAS AND ANDREW B. HECKERT New Mexico Museum of Natural History and Science, Mountain Rd. NW, Albuquerque, NM ABSTRACT.—A nearly 3-km-thick section of Mesozoic sedimentary rocks is exposed at Durango, Colorado. This section con-. The aim of the book is to give an updated overview of the geology of the Arctic sedimentary basins and their petroleum potential. Although the different basins vary significantly as regards sedimentary fill and tectonic evolution, many of the basins share some of the characteristics needed to become prolific oil and gas provinces.

They are situated near the geographic center of the Canadian Arctic Archipelago and encompass the north magnetic pole. Most of the area is covered by sedimentary rocks of Ordovician to Late Devonian age, with a composite exposed thickness of approximat feet.   5. Summary and Conclusions. 1. The Lomonosov Ridge is a continuous band of continental crust extending across the Arctic Ocean from just north of Greenland to the Siberian continental margin (Figures 1 2–3) [e.g., Sweeney et al., ; Forsyth and Mair, ; Jokat et al., ]. It separates the Mesozoic Amerasian Basin from the Cenozoic. Book Chapter (1) Article Type. Facet list. Research Article Canadian Journal of Earth Sciences Arctic Archipelago (2) Liard River (1) Mackenzie Mountains (1). Stratigraphy of Cretaceous - Tertiary rocks of North Bylot Trough, Bylot Island, N.W.T. Geological Survey of Canada, Paper D, pp. – Canada-Nunavut Geoscience Office Summary of Activities, 93 Okulitch, A.V. Geology of the Canadian Arctic Archipelago, Northwest Territories and North Greenland. Geological Survey of.

Higher order eustatic sequences show a significant increase in the number identified. A good portion of the European Mesozoic and Cenozoic succession is set in a sequence stratigraphic context with a better stratigraphic record of its bonding surfaces. MAIN LIBRARY. Perry-Castañeda Library East 21st St. Austin, TX. Phone: () Mesozoic and Cenozoic Sequence Stratigraphy of European Basins (SEPM Special Publication No. 60) [Graciansky, Pierre-Charles de, Hardenbol, Jan, Jacquin, Thierry, Vail, Peter] on *FREE* shipping on qualifying offers. Mesozoic and Cenozoic Sequence Stratigraphy of European Basins (SEPM Special Publication No. 60)Author: Pierre-Charles de Graciansky, Jan Hardenbol, Thierry Jacquin. North America is a continent entirely within the Northern Hemisphere and almost all within the Western can also be described as a northern subcontinent of the Americas, or America, in models that use fewer than seven continents. It is bordered to the north by the Arctic Ocean, to the east by the Atlantic Ocean, to the west and south by the Pacific Ocean, and to the southeast by.

Summary Account of Mesozoic and Tertiary Stratigraphy, Canadian Arctic Archipelago. by Geological Survey of Canada. Download PDF EPUB FB2

The Canadian Arctic Rift System is a major North American geological structure extending from the Labrador Sea in the southeast through Davis Strait, Baffin Bay and the Arctic Archipelago in the northwest.

It consists of a series of interconnected rifts that formed during the Paleozoic, Canadian Arctic Archipelago. book and Cenozoic eras. Extensional stresses along the entire length of the rift system have resulted in Age: Paleozoic-to-Cenozoic.

THE PRESENCE of Mesozoic and Tertiary rocks in the Canadian Arctic Archipelago has been known for many years. Jurassic fossils were the first to be found, by Sir Leopold M’Clintock inwhile searching for Sir John Franklin (Haughton, ).

Get this from a library. Mesozoic and Tertiary geology of Banks Island, Arctic Canada: the history of an unstable craton margin. [Andrew D Miall; Geological Survey of Canada.] -- The main object of this investigation is to demonstrate, through a combination of surface and subsurface stratigraphic data and detailed facies and paleocurrent studies, that sedimentation was.

These Tertiary to Upper Cretaceous strata are part of the Arctic Continental Terrace Wedge province which occurs along the northwestern part of the archipelago (Fig.

1) and which represents the. The Canadian Arctic Islands and nearby mainland areas (Fig. 1) form a physiographic transition between the Atlantic and Arctic Oceans. Thus, the margins of Cited by: Summary account of Mesozoic and Tertiary stratigraphy, Canadian arctic archipelago / by E.T.

Tozer; Mesozoic and Tertiary stratigraphy at Lake Hazen, Northern Ellesmere Island, District of Franklin [by] A The Mesozoic / edited by M. Moullade and A. Nairn; Mesozoic and Tertiary stratigraphy, western Ellesmere Island and Axel Heiberg Island, District of Frankl. The late Tertiary – Quaternary stratigraphic record of the Duck Hawk Bluffs, Banks Island, Canadian Arctic Archipelago February Canadian Journal of Earth Sciences 20(11) stratigraphic methodology because I found I could not apply the methods and terminology proposed by Exxon scientists almost 20 years ago.

As a stratigrapher for the Geological Survey of Canada, my main focus is on the description and interpretation of the Mesozoic succession of the Canadian Arctic Archipelago. Sequence. The Sverdup Basin in the Canadian Arctic archipelago contains 20 discoveries concentrated in the western part of the basin, with resources totalling 3 Bbbloe, predominantly gas.

The sandstone reservoirs range from the Lower Triassic to the Cretaceous with the most important being Upper Triassic to Lower Jurassic (Embry). Some fields have. Book: All Authors / Contributors: Gilbert O Raasch.

Find more information about: Summary account of Mesozoic and Tertiary stratigraphy, Canadian Arctic Archipelago \/ E.T. Tozer -- Pleistocene geology of Arctic Canada \/ B.G.

Craig and J.G. Fyles. Summary account of Mesozoic and Tertiary stratigraphy, Canadian Arctic Archipelago. Geol. Surv. Can., Pap.,24 pp. Tozer, E.T., Mesozoic and Tertiary stratigraphy, western Ellesmere Island and Axel Heiberg Island, District of A S H T O N F.

EMBRY Institute of Sedimentary and Petroleum Geology, rd Street, N. W, Calgary. Quaternary glacial chronology of the eastern Canadian Arctic: A review and a contribution on Amino acid dating of Quaternary molluscs from the Clyde Cliffs. 1 – 32 in Mahaney, W.C. (Ed.), Quaternary Stratigraphy of North America.

A revised biostratigraphic and well-log sequence-stratigraphic framework for the Scotian Margin, offshore eastern Canada. 1 This article is one of a series of papers published in this CJES Special Issue on the theme of Mesozoic–Cenozoic geology of the Scotian Basin.

Mesozoic Era: Stratigraphy You can find out more about the Mesozoic by clicking on the chart below. Find out more about the Mesozoic paleontology and geology of North America at the Paleontology Portal.

Geological setting of Sverdrup basin The detailed Mesozoic history of the Canadian Arctic Islands, in terms of stratigraphy, sedimentation and depositional history, is described by Embry ( 1). Figure 2 shows the distribution and thickness of Mesozoic strata, including total well control in Sverdrup Basin (Figure 2a) and a number of wells in.

Abstract. The early Tertiary southern Arctic was an important biogeographic exchange route between the Old and New Worlds.

A variant of the nearest living relative method of paleoclimatic estimation suggests that the mean temperature of the coldest month of the Eocene southern Arctic was about 10 °C, with the possibility of limited frost. In Geology of the Innuitian Orogen and Arctic Platform of Canada and Greenland, H.P.

Trettin (ed.). Geological Survey of Canada, Geology of Canada, no. 3, p. Thorteinsson, R. Carboniferous and Permian stratigraphy of Axel Heiberg Island and western Ellesmere Island, Canadian Arctic Archipelago. The tectonic framework and depositional settings of the Orphan Basin are studied using ~25, km of 2-D seismic reflection profiles and stratigraphic data from nine key exploration wells.

The evolution of the region is recorded in five seismic distinct stratigraphic units (Z, A, B, C, X), each separated from one another by widespread regional markers U1-U4, representing prominent unconformities.

The general geology of the islands of the Arctic Archipelago has been described and mapped on a small scale by the Geological Survey of Canada, but the detailed geology is known in only a very few small areas.

Systematic mapping of the region has hardly begun. Only a general account of the geology. Henderson, C.M. Conodont paleontology and biostratigraphy of the Upper Carboniferous to Lower Permian Canyon Fiord, Belcher Channel, Nansen, and Van Hauen formations and an unnamed formation, southwestern Ellesmere Island, Canadian Arctic Archipelago.

Unpublished Ph.D. thesis, University of Calgary, p. Henderson, C.M. The Cretaceous to Paleogene High Arctic Large Igneous Province (HALIP) occurs in circum-Arctic regions, and the largest portion of the province occurs in Canada’s Arctic Archipelago.

This paper reviews and documents the geometry and distribution of the Canadian portion of the HALIP, focussing most notably on the architecture of its intrusive.

Summary. The geographic pattern of the Atlantic Canada coastal geomagnetic induction anomaly is delineated using both the vertical transfer function and the at Heat flow determinations in the Canadian Arctic Archipelago, Can. earth Sci., 2, 59 Cenozoic and Mesozoic stratigraphy of the Scotian Shelf, Can.

earth Sci., 9, Dinocyst stratigraphy of the Valanginian–Aptian Rurikfjellet and Helvetiafjellet formations on -Hansen, H and McIntyre, DJ () Upper Barremian to Upper Albian (Lower Cretaceous) dinoflagellate cyst assemblages, Canadian Arctic Archipelago.

Palynol – Mesozoic–Tertiary dinoflagellates, acritarchs and prasinophytes. P / Thorsteinsson, R. and Tozer, E. / SUMMARY ACCOUNT OF STRUCTURAL HISTORY OF THE CANADIAN ARCTIC ARCHIPELAGO SINCE PRECAMBRIAN TIME, Ottawa,pb, 25 pages, 4 figs.

(2 in pocket), - 5 - $ You can write a book review and share your experiences. Other readers will always be interested in your opinion of the books you've read.

Whether you've loved the book or not, if you give your honest and detailed thoughts then people will find new books that are right for them. Purchase Arctic Geology and Petroleum Potential, Volume 2 - 1st Edition. Print Book & E-Book. ISBNLexicon of Canadian stratigraphy. -- by,Canadian Society of Petroleum Geologists edition, in English.

Neogene sediments in the Canadian Arctic Archipelago” In other words, the date and formation simply filled a time Summary The Arctic coastal plain sediments of North America are Canadian Arctic islands: Late Tertiary sandy braided river deposits with woody detritus beds, Arctic 44(3)–, English summary] Kemper, E.

Upper Deer Bay formation (Berriasian-Valanginian) of Sverdrup Basin and P.R. Mesozoic stratigraphy in the Blue Mountains and Krieger Mountains, northern Ellesmere Island, Arctic Canada: A preliminary account.

and rotations in the Canadian Arctic archipelago. Geophys. Res.: Sol. Earth, The stratigraphic sequence breakdown was determined in except on Banquereau C21, Thebaud I93 and Venture B For these three wells, the stratigraphic breakdown was performed by correlation with nearby wells (Figure 1; PL.

and ). Up to five, second order stratigraphic sequences, with average duration of Ma, are defined from. Summary This chapter contains sections titled: Precursor Events Triassic Jurassic Cretaceous Tertiary Mesozoic and Cenozoic Structure and Stratigraphy of the San Juan Basin: An Overview - Condon - - Field Trip Guidebooks - Wiley Online Library.

Numerical modelling is used to investigate for the first time the interactions between a petroleum system and sill intrusion in the NE Sverdrup Basin, Canadian Arctic Archipelago. Although hydrocarbonexploration has been successful in the western Sverdrup Basin, the results in the NE part of thebasin have been disappointing, despite the presence of suitable Mesozoic source rocks.Paleozoic and Mesozoic stratigraphy of the northern part of the Ruby Range, southwestern Montana.

(Contributions to stratigraphy) (Geological Survey Bulletin ) and Tertiary -rocks at the northern tip of the range were noted briefly in a report of Fields and Petkewich ().