Mesozoic deposits of the Hudson Bay Lowlands and coal deposits of the Onakawana area, Ontario
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Mesozoic deposits of the Hudson Bay Lowlands and coal deposits of the Onakawana area, Ontario

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

Subjects:

  • Hudson Bay Lowlands,
  • Onakawana lignite

Book details:

Edition Notes

11

The Physical Object
Pagination39 p.
Number of Pages39
ID Numbers
Open LibraryOL22012116M

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The Cambrian spanned from to million years ago and is the first period of the Paleozoic era of the Phanerozoic. The Cambrian marked a boom in evolution in an event known as the Cambrian explosion in which the largest number of creatures evolved in any single period of the history of the Earth. Creatures like algae evolved, but the most ubiquitous of that period were the armored. Cretaceous fluvial strata in the Moose River Basin of Ontario, Canada, as a source of kaolin for paper and ceramic industries January Applied Clay Science 16(1) The Hudson Bay-Arctic Lowlands is a landform region of Canada, located more specifically in Ontario, Quebec, Manitoba, Yukon, Northwest Territories, and Nunavut. This region formed in the Paleozoic Era, when the enormous weight of a glacier sunk the Canadian Shield and the area became lowlands when the glaciers retreated. Western Canada during the Mesozoic The Mesozoic extends over million years from the beginning of the Triassic ( Ma) to the end of the Cretaceous (65 Ma). It was a particularly important period for the geology of western Canada.

Nicolas, M.P.N. and Lavoie, D. Oil shale and reservoir rocks of the Hudson Bay Lowland, northeastern Manitoba (part of NTS 54); in Report of Activities , Manitoba Innovation, Energy and Mines, Manitoba Geological Survey, p. – Summary The Hudson Bay and Foxe Basins Project is in its fourth and final year. The Trout Lake deposit ( ± 1 Ma) is a rhyolite-hosted, bimodal-mafic, volcanogenic massive sulfide (VMS) deposit. It is one of the largest VMS deposits in the Flin Flon mining district, containing Mt of Cu-Zn rich ore. The deposit underwent greenschist facies metamorphism and polyphase synvolcanic to postvolcanic hydrothermal alteration. morphology and depositional environment. Unlike most other coal deposits in Saskatchewan, which are relatively thin (less than a few metres), regionally extensive paralic-type deposits, the Hudson Bay area coal discoveries are more localized and have far greater thicknesses of up to m (including partings). Prior to retirement Darrel G.F. Long worked in the PhD Program in Mineral Deposits and Precambrian Geology, Laurentian University. Darrel does research in Fluvial Sedimentology, Stratigraphy.

Chronology, Paleoecology and Stratigraphy of Late Pleistocene Sediments from the Hudson Bay Lowlands, Canada April Sue Rogers Dalton Doctor of Philosophy in Earth Sciences Department of Earth Sciences University of Toronto Abstract Stratigraphic records in the Hudson Bay Lowlands (HBL), Canada, offer rare insight into local. Figure 1: Hudson Bay Lowlands in northeastern Manitoba, showing the location of the cores available; inset is the project area for the GEM Hudson Bay and Foxe Basins Project. Figure 4: Stratigraphy of the Hudson Bay Lowlands, with correlations to the Manitoba Hydro units; Ordovician System/Stages from Zhang and Barnes (). black shales, and coal. These deposits represent the diverse fluvial to deltaic and lacustrine environments that existed within the basins. The rifting ended early in the Jurassic with the onset of regional volcanism and intrusion of diabase dikes and sills. Source Rocks The source rocks for oil and gas within the Mesozoic basins include the. Deformed Mesozoic volcanogenic Cu-Zn sulfide deposits in the Britannia District, British Columbia; discussion Glenn C. Waterman P.O. Box , Freeland, WA, United States.