2 edition of Dolomitization in the Trenton of south-western Ontario. found in the catalog.
Dolomitization in the Trenton of south-western Ontario.
Written in English
Thesis (M.A.) -- University of Toronto, 1948.
|The Physical Object|
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impacts of climate change are discussed for the region of Canada with a focus on South-Western Ontario. Literature review According to IPCC, () any detectable change in the state of climate which persists over a considerable period of time (more than a decade) can be referred to as climate change.
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% Effect of silica content on clinker : S.P. Ghosh. - Early dolomitization and recrystallization of carbonate in an evaporite basin: the Middle Devonian Ratner laminite in southern Saskatchewan, Canada.
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Full text of "Prospector's field-book and guide; in the search for and the easy determination of ores and other useful minerals" See other formats. Hydrothermal Dolomitization and a Fluid Flow Model: An Example from the Middle Ordovician Trenton Group, southwestern Ontario, Canada Han, Jiajun* ; Mirko van der Baan Seismic Time-Frequency Analysis by Empirical Mode Decomposition.
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Shaughnessy, AB: Standard coal mine becomes the Galt No. 10 with the closure of Galt No. Michigan Geology: A Bibliography Peter Voice PhD January, 54th Annual Meeting of the Institute on Lake Superior Geology Guide Book (Ed.
by T. Bornhorst & J. Klasner), 54, CANNON, W.F., LABERGE, G.L., KLASNER, J.S. & SCHULZ, K.J. () The Gogebic Iron Range - a Sample of the Northern Margin of the Penokean Fold and. THOMAS R. TAYLOR and DUNCAN F.
SIBLEY - Petrographic and geochemical characteristics of dolomite types and the origin of ferroan dolomite in the Trenton Formation, Ordovician, Michigan Basin, U.S.A. - Sedimentology 33; pp.illustr. Orig.
extract, very good. € 5.Visible-near infrared - shortwave infrared (VNIR-SWIR) spectroscopy, gamma-ray logs, and magnetic susceptibility measurements were taken on drill core samples that span the Patterson Lake exploration corridor (PLC) on the south-western margin of the Athabasca Basin.Evidence concerning the ecology of American Palaeozoic sponges, excluding hexactinellids and incertae sedis, is discussed and evaluated.
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