Appalachian stratigraphy and structure of the Maritime Provinces from Halifax to Chaleur Bay

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Published by International Geological Congress in Montreal .

Written in English

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Open LibraryOL22013773M

Download Appalachian stratigraphy and structure of the Maritime Provinces from Halifax to Chaleur Bay

This is a non-technical book suitable for amateur geologists that has lots of pictures and diagrams. Most interesting to me was the discussion of the supercontinent before Pangaea and how its history is reflected in the rocks of Nova Scotia and the other maritime provinces of Canada.4/5(8).

STRATIGRAPHY Overview PL. Regional Geology and Stratigraphic Framework Overview The Sable Sub-basin corresponds to the central slope of the Scotian Margin and has been the main focus of offshore oil and gas exploration in Nova Scotia, with several commercial discoveries since the s leading to the development of the Sable OffshoreFile Size: 8MB.

Acadian Geology: An Account Of The Geological Structure And Mineral Resources Of Nova Scotia And Portions Of The Neighbouring Provinces Of British America [Dawson, John William] on *FREE* shipping on qualifying offers.

Acadian Geology: An Account Of The Geological Structure And Mineral Resources Of Nova Scotia And Portions Of The Author: John William Dawson.

Retreat of the last ice sheet from the Maritime Provinces - Gulf of St. Lawrence region; Geological Survey of Canada, Paper15 p. Prest, W. H., Glacial succession in central Lunenburg, Nova Scotia; Proceedings and Transactions of the Nova Scotian Institute of Science, Halifax, v.

9, sessionp. Stratigraphy and sedimentology of early Pennsylvanian red beds P.O. BoxHalifax, Nova Scotia, B3J 2T9, Canada Appalachian mountains and midway between the Appalachian. The last three are traditionally known as the “Maritime Provinces.” The four comprise a more or less distinct morphotectonic division–the Canadian sector of the Appalachian orogenic belt, although a narrow part of the latter also extends along.

Details of the stratigraphy of TS IV are given below in discussion of the GAV core. Figure 4: Tectonstratigraphy and age of the Argana and Fundy basins (modified from Olsen et al., ).

Note that the members of the Fundy basin are presently informal units, with the exception of the Scots Bay Member (Tanner, ). This profile illustrates the stratigraphy beneath northern Cape Cod Bay offshore of Duxbury Beach and Plymouth Bay, Massachusetts, seaward of profile E–E′ in figure Deep fluvial channels incised into the surface of thick glaciolacustrine (Qdl) sediments are filled with Holocene fluvial and estuarine (Qfe) deposits.

The stratigraphy of the Windsor group in the Antigonish quadrangles and the Mahone Bay-St. Margaret Bay area, Nova Scotia Article March with 7 Reads How we measure 'reads'. Carboniferous Maritime Basin The Late Paleozoic Maritimes Basin of Atlantic Canada is an extensive successor basin that formed in the wake of the Early to Middle Devonian Acadian Orogeny.

In New Brunswick the basin is characterized by thick accumulations of dominantly sedimentary rocks deposited in alluvial, fluvial, lacustrine and marine.

The mainland portion of the Nova Scotia peninsula is attached to North America through the Isthmus of s offshore islands, the largest of which is Cape Breton Island, form the bulk of the eastern part of the province. The geological history of the province spans more than billion years.

Continental drift led to the southern half of the province's mainland. per Windsor age are present on Mira Bay, on the upper part of Sydney River, on the borders of Coxheath upland, and probably again as the St. Ann formation on St.

Ann bay". The writer'sobservations in the Mabou-]udiquc area indicate a thickness of the \Vindsor of the order of magnitude of 2, to 2,'.

Sandra Barr is a faculty member in the Department of Earth and Environmental Science at Acadia University in Wolfville. Widely recognized as an expert in the geology of Nova Scotia, she is also co-editor of the scientific journal Atlantic Geology, and is book editor for the Geological Association of Canada/5(7).

ATLAS of the MARITIME PROVINCES of the DOMINION OF CANADA, With Historical and Geological Descriptions. Author, etc. Duncan Campbell James Fowler. Description. One of the few atlases we've seen from the 19th century where attribution to the sources used is given (see subtitle).

Publisher. Roe Brothers. Place of Publication. Maine Geological Survey. Includes technical papers on C.T. Jackson, the lithotectonic stratigraphy of the Casco Bay region, early premetamorphic faults in western Maine, the shale-wacke sequence in south-central Maine, a Silurian unconformity at Flanders Bay, Devonian deltaic sedimentary environments of the Matagamon Sandstone, the occurrence of the crinoid Cited by: 3.

Published by Nimbus Publishing - Paper The first contemporary book written for the general reader on the geological history of the Maritime Provinces.

This book is beautifully illustrated in full colour, with original paintings of ancient vistas, over photographs, and crisp explanatory diagrams and sketches. Acadian geology [microform]: an account of the geological structure and mineral resources of Nova Scotia and portions of the neighbouring provinces of British America by Dawson, J.

(John William), Sir, Pages:   Open Library is an open, editable library catalog, building towards a web page for every book ever published. Lexicon of Canadian stratigraphy. -- by,Canadian Society of Petroleum Geologists edition, in English. The well was drilled in 90 m ( ft) of water, km ( mi) southeast of Halifax, Canada.

Subsequent delineation and development drilling has proven a significant gas accumulation. The gas is trapped, by a combined structural-stratigraphic configuration, in the Upper Jurassic reefal and oolitic limestones and dolomites of the Abenaki Formation.

Revised Upper Cretaceous and lower Paleogene lithostratigraphy and depositional history of the Jeanne d'Arc Basin, offshore Newfoundland, Canada Dalhousie University, Halifax, Nova Scotia, Canada, outreach, and the geological history of the Maritime Provinces of Canada, recently coediting a book on the last subject (with Graham Williams).

The Geology Collections of the Nova Scotia Museum tell the labyrinthine story of the geological history of the province through representative rocks, minerals, gemstones, and fossils (vertebrate, invertebrate, palaeobotanical and traces). The Geology Collections also include comparative rocks, minerals, gemstones, meteorites and fossils from across Canada and around the world.

The Maritimes Basin comprises a complex suite of upper Paleozoic strata that cover a large onshore and offshore area of eastern Canada. As presently preserved, the basin extends about km from southwestern New Brunswick to the continental margin on the eastern Grand Banks, and about km from the southern Grand Banks to offshore Labrador ().Author: M.R.

Gibling, N. Culshaw, V. Pascucci, J.W.F. Waldron, M.C. Rygel. These members record two main progradational episodes that are separated by a regional unconformity and a thick shale interval corresponding to the Bay Bulls Member. East of the shelf-slope system, Upper Cretaceous shale and sparse sandstone of the Dawson Canyon Formation and chalk of the Petrel Member and Wyandot Formation were deposited in a Cited by: Start studying World Geography chapter 6- Canada.

Learn vocabulary, terms, and more with flashcards, games, and other study tools. Image 4 of Volume 2 E L By the same Author. A SECOND VISIT TO THE UNITED STATES, –6. Third Edition. 2 vols. Post 8vo. 12 s. Sedimentology, stratigraphy, and structure of the late cretaceous rocks of Mayne and Samuel Islands, British ColumbiaCited by: 1.

Detailed mapping and structural investigations in an area bound to the west by the Grenvillian basement of the Adirondack Mountains and to the east by the allochthonous slates of the Taconic Mountains led to the distinction of a Western Undeformed Zone and an Eastern Deformed Zone.

The former is composed of the gently east-dipping shelf sequence of upper Cambrian to lower Cited by: 1. CHS offers charts, covering all three of Canada's coastlines plus major inland waterways.

Canadian Nautical Charts Atlantic Region Halifax Harbour - Point Pleasant to. The Gulf of Maine, sometimes referred to as a “sea within a sea,” extends 7, miles from Cape Cod to Cape Sable, Nova Scotia.

The region’s boundaries are divided between three New England states: Massachusetts, New Hampshire and Maine; and two Maritime provinces: New Brunswick and Nova Scotia (Fig.1).

Maps Showing the Stratigraphic Framework of South Carolina's Long Bay from Little River to Winyah Bay USGS Open File Report by: Wayne E. Baldwin, Robert A. Morton, Jane F. Denny, Shawn V. Dadisman, William C. Schwab, Paul T. Gayes, and Neal W. Driscoll. Chapter 9 Sedimentology of braided-river deposits in Upper Triassic Wolfville redbeds, southern shore of Cobequid Bay, Nova Scotia, Canada JOHN F.

HUBERT and MICHAEL F. FORLENZA ABSTRACT During Late Triassic time, the m of Wolfville redbeds accumulated in a semiarid rift valley near 20°N by: The Upper Carboniferous Stratigraphy of the UK and Dutch Sectors: Southern North Sea Phase 1 (NE) A Chemostratigraphic and Palynological evaluation of 49 wells from the Upper Carboniferous of the UK and Dutch Southern North Sea.

Quads: 44, 49, D, E, F, K. Stratigraphic Range: Bashkirian to Gzhelian (Upper Carboniferous), Lower Permian. Seismic sequence stratigraphy during the Cretaceous through the early Paleogene in the northern Scotian basin (Laurentian Subbasin) offshore Nova Scotia and Newfoundland, Canada.

PDF. PDF format is widely accepted and good for printing. Plug-in required. PDF-1 ( MB) Citation & Export. View Usage Statistics. Staff View. Temperatures and densities of the waters of eastern Canada, including the Atlantic from the bay of Fundy to Newfoundland; the gulf of St.

Lawrence, and the straits connecting it with the ocean. Canada. Dept. of Naval Service Dawson, William Bell, Type. Book Material. Published material. Publication info. Start studying Géoculture: La province de Québec.

Learn vocabulary, terms, and more with flashcards, games, and other study tools. Chemostratigraphy of the Upper Carboniferous Schooner Formation, southern North Sea T. Pearce, 1 D. Wray, 2 K. Ratcliffe, D. Wright, 1 A.

Moscariello 3 1. Carbonate and Siliciclastic Sequence Stratigraphy - Examples from the Late Jurassic Abenaki Limestone and West Venture Deltai c Beds, Offshore Nova Scotia, Canada Leslie Eliuk * Dalhousie University Earth Sciences, Halifax, Nova Scotia, Canada [email protected] and Grant Wach Dalhousie University Earth Sciences, Halifax, Nova Scotia, CanadaFile Size: 1MB.

Description The Scotian basin is a postrift basin on the passive margin of eastern North America. Using 2D and 3D seismic data, located in the Laurentian and Penobscot study areas, respectively, I have identified three types of deformation affecting Cretaceous through Recent strata: reactivation of basement-involved faults during both extensional and contractional.

CHS offers charts, covering all three of Canada's coastlines plus major inland waterways. Canadian Nautical Charts Atlantic Region Cabot Strait and approaches - Detroit de Cabot et les approches, Scatarie Island to-a Anticosti Island - Ile D'Anti.

Abstract: Multiscale Characterization of a Marine Shelf Sandstone, the Cardium Formation in the Wapiti Field, Alberta Basin, Canada. SOCAS-BASSONS, MERCEDES, and COLIN P. NORTH, University of Aberdeen; Mark Savage, Petro-Canada Oil and Gas.

A new seismic stratigraphy in the Indian-Atlantic Ocean gateway resembles major paleo-oceanographic changes of the last 7 Ma Sea-level and surface-water change in the western North Atlantic across the Oligocene-Miocene Transition: A palynological perspective from IODP Site U (Newfoundland margin).Name Geological Survey of Canada (Atlantic) Main Location Challenger Drive, Dartmouth, Canada Categories Associations Telephone Main: () Follow us.Hudson Bay drainage basin, and is located at the western end of the Moose River Basin (Fig.

). Both the Ridge and Squirrel rivers drain west into the Kenogami and north until it converges with the Albany River before flowing into Hudson Bay. The Pivabiska drains east into the Missinaibi River before entering Hudson Bay via the Moose River.

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