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Lavoie, Denis, Malo, Michel, Tremblay, Alain (2003) The Cambrian–Ordovician successions along the ancient continental margin of Laurentia — recent advances. Canadian Journal of Earth Sciences, 40 (2) 131-133 doi:10.1139/e03-013

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Reference TypeJournal (article/letter/editorial)
TitleThe Cambrian–Ordovician successions along the ancient continental margin of Laurentia — recent advances
JournalCanadian Journal of Earth Sciences
AuthorsLavoie, DenisAuthor
Malo, MichelAuthor
Tremblay, AlainAuthor
Year2003 (February 1)Volume40
Issue2
PublisherCanadian Science Publishing
DOIdoi:10.1139/e03-013Search in ResearchGate
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Mindat Ref. ID483785Long-form Identifiermindat:1:5:483785:9
GUID0
Full ReferenceLavoie, Denis, Malo, Michel, Tremblay, Alain (2003) The Cambrian–Ordovician successions along the ancient continental margin of Laurentia — recent advances. Canadian Journal of Earth Sciences, 40 (2) 131-133 doi:10.1139/e03-013
Plain TextLavoie, Denis, Malo, Michel, Tremblay, Alain (2003) The Cambrian–Ordovician successions along the ancient continental margin of Laurentia — recent advances. Canadian Journal of Earth Sciences, 40 (2) 131-133 doi:10.1139/e03-013
In(2003, February) Canadian Journal of Earth Sciences Vol. 40 (2) Canadian Science Publishing
Abstract/Notes The Appalachian Forelands and Platform NATMAP project in eastern Canada is a multi-discipline and multi-organization research endeavour aimed at the understanding of the evolution and architecture of the ancient continental margin of Laurentia. The Canadian Journal of Earth Sciences special issue presents some recent research progress for our knowledge of the CambrianOrdovician segment of that ancient margin.

See Also

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Lavoie, Denis, Malo, Michel, Tremblay, Alain (2004) The Late Ordovician – Middle Devonian Gaspé Belt in eastern Canada — recent advances. Canadian Journal of Earth Sciences, 41 (5) 483-487 doi:10.1139/e04-033
Lavoie, Denis, Burden, Elliott, Lebel, Daniel (2003) Stratigraphic framework for the Cambrian–Ordovician rift and passive margin successions from southern Quebec to western Newfoundland. Canadian Journal of Earth Sciences, 40 (2) 177-205 doi:10.1139/e02-078
Lemieux, Yvon, Tremblay, Alain, Lavoie, Denis (2003) Structural analysis of supracrustal faults in the Charlevoix area, Quebec: relation to impact cratering and the St-Laurent fault system. Canadian Journal of Earth Sciences, 40 (2) 221-235 doi:10.1139/e02-046
Lavoie, Denis (1994) Diachronous tectonic collapse of the Ordovician continental margin, eastern Canada: comparison between the Quebec Reentrant and St. Lawrence Promontory. Canadian Journal of Earth Sciences, 31 (8) 1309-1319 doi:10.1139/e94-113
Pincivy, Alix, Malo, Michel, Ruffet, Gilles, Tremblay, Alain, Sacks, Paul E (2003) Regional metamorphism of the Appalachian Humber zone of Gaspé Peninsula: 40Ar/39Ar evidence for crustal thickening during the Taconian orogeny. Canadian Journal of Earth Sciences, 40 (2) 301-315 doi:10.1139/e02-076
Castonguay, Sébastien, Tremblay, Alain (2003) Erratum: Tectonic evolution and significance of Silurian – Early Devonian hinterland-directed deformation in the internal Humber zone of the southern Quebec Appalachians. Canadian Journal of Earth Sciences, 40 (4) 679 doi:10.1139/e03-901
Faure, Stéphane, Tremblay, Alain, Malo, Michel (2004) Reconstruction of Taconian and Acadian paleostress regimes in the Quebec and northern New Brunswick Appalachians. Canadian Journal of Earth Sciences, 41 (5) 619-634 doi:10.1139/e04-020
Lavoie, Denis, Chi, Guoxiang (2010) An Ordovician “Lost City” — venting serpentinite and life oases on Iapetus seafloor. Canadian Journal of Earth Sciences, 47 (3) 199-207 doi:10.1139/e10-013
Malo, Michel (2004) Paleogeography of the Matapédia basin in the Gaspé Appalachians: initiation of the Gaspé Belt successor basin. Canadian Journal of Earth Sciences, 41 (5) 553-570 doi:10.1139/e03-100
Behncke, Boris, Neri, Marco (2003) Cycles and trends in the recent eruptive behaviour of Mount Etna (Italy) Canadian Journal of Earth Sciences, 40 (10) 1405-1411 doi:10.1139/e03-052
Lavoie, Denis (1992) Peritidal origin of the Lower Ordovician Upton Group, southern Quebec Appalachians. Canadian Journal of Earth Sciences, 29 (5) 1106-1118 doi:10.1139/e92-088
 
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