The Late Ordovician Dawson Point Formation (Timiskaming outlier, Ontario): key to a new regional synthesis of Richmondian–Hirnantian carbonate and siliciclastic magnafacies across the central Canadian craton.
Autor: | Dix, George R.1 gdix@ccs.carleton.ca, Coniglio, Mario2, Riva, John F. V.3, Achab, Aïcha3 |
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Zdroj: | Canadian Journal of Earth Sciences. Sep2007, Vol. 44 Issue 9, p1313-1331. 19p. 6 Color Photographs, 6 Black and White Photographs, 7 Diagrams, 2 Maps. |
Databáze: | Academic Search Ultimate |
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