Relevant bibliographies by topics / Gaspé Peninsula

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  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Reports

Academic literature on the topic 'Gaspé Peninsula'

Author: Grafiati
Published: 4 June 2021
Last updated: 1 February 2022

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Journal articles on the topic "Gaspé Peninsula"

1

D’hulst, Alan, Georges Beaudoin, Michel Malo, Marc Constantin, and Pierre Pilote. "Geochemistry of Sainte-Marguerite volcanic rocks: implications for the evolution of Silurian–Devonian volcanism in the Gaspé Peninsula." Canadian Journal of Earth Sciences 45, no. 1 (2008): 15–29. http://dx.doi.org/10.1139/e07-012.

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The Lower Devonian Sainte-Marguerite volcanic rocks are part of a Silurian–Devonian volcanic sequence deposited between the Taconian and Acadian orogenies in the Gaspé Peninsula, Quebec, Canada. The Sainte-Marguerite unit includes basaltic and dacitic lava flows with calc-alkaline and volcanic-arc affinities. Such affinities are also recorded by the trace-element signature in Lower Silurian and most Lower Devonian volcanic units of the Gaspé Peninsula. However, most of the other Silurian–Devonian volcanic rocks occurring in the Gaspé Peninsula have been previously interpreted to have erupted i
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Belland, René J., and Marc Favreau. "The moss flora of the Gaspé Peninsula (Quebec, Canada): list of species and preliminary analysis." Canadian Journal of Botany 66, no. 9 (1988): 1780–99. http://dx.doi.org/10.1139/b88-244.

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Extensive field studies and evaluation of previously published reports reveal a moss flora of at least 310 species for the Gaspé Peninsula. Forty species are reported for the first time from the peninsula, and Brachythecium glaciale is new to Quebec. While the Gaspé flora cannot be considered a distinctive one within the Gulf of St. Lawrence region, the large number of rare species is significant. Their presence in the Gaspé can be attributed to the diverse geology and topography of the peninsula. The bulk of the moss flora is clearly of boreal affinity, but many species have temperate, montan
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Lavoie, Denis. "The Lower Devonian Compton Formation in southern Quebec: from delta front to pro-delta sedimentation." Canadian Journal of Earth Sciences 41, no. 5 (2004): 571–85. http://dx.doi.org/10.1139/e04-026.

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The Lower Devonian Compton Formation is the uppermost unit of the St. Francis Group in the Connecticut Valley – Gaspé synclinorium of southern Quebec. The Compton Formation is composed of three informal members. Five distinct sedimentary facies have been recognized in the lower two members of the Compton Formation. High-energy, shallow-marine, and channel sands dominate the Milan member. The overlying Lac Drolet member consists of below wave base mud and silt deposits with abundant turbidite sand. The Milan member is interpreted to represent deposits of a river-dominated delta-front environmen
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Malo, Michel, Donna Kirkwood, Gilles De Broucker, and Pierre St-Julien. "A reevaluation of the position of the Baie Verte – Brompton Line in the Quebec Appalachians: the influence of Middle Devonian strike-slip faulting in Gaspé Peninsula." Canadian Journal of Earth Sciences 29, no. 6 (1992): 1265–73. http://dx.doi.org/10.1139/e92-101.

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The Baie Verte – Brompton Line (BBL), the surface expression of the Taconian suture in the Canadian Appalachian Orogen, extends from southern Quebec to the northeast end of Newfoundland. In the Quebec Appalachians, the BBL was previously located under the post-Taconian cover rocks between the Eastern Townships and Gaspé Peninsula. New geological data and reinterpretation of gravimetric and aeromagnetic data suggest that the BBL follows the southern edge of the Cambrian–Ordovician rocks of northern Gaspé Peninsula and is displaced by Middle Devonian strike-slip faults on the southern part of th
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Lavoie, Denis. "Carbonate sedimentation in an extensional tectonic regime: the Lower Devonian Upper Gaspé Limestones, Quebec Appalachians." Canadian Journal of Earth Sciences 29, no. 1 (1992): 118–28. http://dx.doi.org/10.1139/e92-012.

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Carbonate sedimentation occurred over most of eastern Gaspé Peninsula in Early Devonian time. The resulting succession, known as the Upper Gaspé Limestones, is a 500–1800 m thick unit outcropping in the Connecticut Valley – Gaspé Synclinorium. Detailed stratigraphic and sedimentologic work allows recognition of important thickness and lithofacies variations in a north–south-oriented transect in the eastern part of the peninsula. Variations are spatially associated with Acadian (Middle Devonian) dextral strike-slip faults. Three lithotectonic domains are proposed and interpreted; they are, from
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6

Riva, John, and Michel Malo. "Age and correlation of the Honorat Group, southern Gaspé Peninsula." Canadian Journal of Earth Sciences 25, no. 10 (1988): 1618–28. http://dx.doi.org/10.1139/e88-154.

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The Honorat Group of southern Gaspé consists of two formations: the Arsenault and the Garin. The Arsenault Formation, heretofore considered barren, has yielded a graptolite faunule indicative of a Llanvirn–Llandeilo age (early Middle Ordovician), suggesting a correlation with the lower Mictaw Group of Gaspé as revised by de Broucker. A hiatus of indeterminate magnitude, corresponding to the Taconic unconformity, probably separates the Arsenault Formation from the overlying Garin Formation. The Garin has yielded graptolites ranging from the upper Climacograptus spiniferus Zone to the Paraclimat
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7

BÉDARD, JEAN H. "Pre-Acadian magmatic suites of the southeastern Gaspé Peninsula." Geological Society of America Bulletin 97, no. 10 (1986): 1177. http://dx.doi.org/10.1130/0016-7606(1986)97<1177:pmsots>2.0.co;2.

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Asselin, Esther, Aïcha Achab, and Azzedine Soufiane. "Biostratigraphic significance of lower Paleozoic microfaunas from eastern Canada." Canadian Journal of Earth Sciences 41, no. 5 (2004): 489–505. http://dx.doi.org/10.1139/e03-094.

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Chitinozoan studies recently carried out in the “Appalachian Forelands and St. Lawrence Platform” National Geoscience Mapping Program (NATMAP) project have confirmed the regional biostratigraphic value of a number of chitinozoan species and led to a better documentation of their stratigraphic and geographic distribution in eastern Canada. The typical Darriwilian microfaunas first described from the Table Head Group of western Newfoundland and containing Conochitina chydaea are now recognised in the Rivière Ouelle Formation at Les Méchins, Gaspé Peninsula. In the Upper Ordovician successions of
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9

Landry, Bernard, and Cees Gielis. "Key to the Paraplatyptilia species of eastern Canada with description of a new species (Lepidoptera: Pterophoridae)." Canadian Entomologist 140, no. 2 (2008): 143–48. http://dx.doi.org/10.4039/n07-026.

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AbstractParaplatyptilia atlanticasp. nov. is described as new from northwestern Newfoundland and the Gaspé Peninsula, Quebec, Canada. A key to the four species of Paraplatyptilia Bigot and Picard known to occur in eastern Canada (east of Manitoba) is provided.
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Jutras, Pierre, Gilbert Prichonnet, and Steven McCutcheon. "Alleghanian deformation in the eastern Gaspé Peninsula of Quebec, Canada." Geological Society of America Bulletin 115, no. 12 (2003): 1538. http://dx.doi.org/10.1130/b25306.1.

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Dissertations / Theses on the topic "Gaspé Peninsula"

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Cashman, Patrick Bradley. "Problematic marine palynomorphs from the Silurian-Devonian Gaspé Limestones, Gaspé Peninsula, Quebec, Canada." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1995. http://www.collectionscanada.ca/obj/s4/f2/dsk3/ftp04/NQ23931.pdf.

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Wallace, Graeme M. B. "Petrogenesis of the McGerrigle plutonic complex, Gaspe, Quebec." Thesis, McGill University, 1988. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=63877.

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Stevens, Kirk. "Fluid inclusion and geological studies on the Zn-Pb-Cu vein system at Lemieux Dome, Gaspe, Quebec." Thesis, McGill University, 1986. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=65412.

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Coulombe, Pontbriand Moise. "Geomorphic controls on the distribution of Atlantic salmon (Salmo salar) habitat in two contrasting fifth-order streams in the Gaspe Peninsula, Quebec : the Petite Cascapedia and Bonaventure rivers." Thesis, McGill University, 2001. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=33743.

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Although the watersheds of the Petite Cascapedia and Bonaventure Rivers, Gaspe Peninsula, have broadly similar geology and land use, their segment-scale river geomorphology is contrasted by subtle differences in valley characteristics that are a legacy of their individual geomorphic histories. These differences have consequences on the distribution of Atlantic salmon habitat such as boulder abundance (for parr rearing and overwintering habitats) and spawning substrate quality. Parr preference for boulder-rich river segments (1--5 km) was observed in the Bonaventure River. In the study systems
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La, Rocque Cynthia A. "Geochronology and petrology of north-central Gaspe igneous rocks, Quebec." Thesis, McGill University, 1986. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=65499.

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Dalton, Edward. "Sedimentary facies and diagenesis of the Lower Devonian Temiscouata and Fortin Formations, Northern Appalachians, Quebec and New Brunswick." Thesis, McGill University, 1987. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=63856.

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Shah, Jehangir A. "Early diagenetic deep-sea dolomites from the middle ordovician cloridorme formation, Gaspé Peninsula, Québec Appalachians and related occurrences." Thesis, McGill University, 1989. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=59231.

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Textural evidence, high carbonate concentration and septarian cracks in dolomite and calcite concretions and beds of the Middle Ordovician Cloridorme and Cow Head formations indicate early carbonate precipitation during very shallow burial in uncompacted or little compacted host-sediments. These carbonates started to form at a depth not exceeding 5 m from the seafloor, where porosities were as high as 90%, and continued to grow in the sediment column to subsurface depth of 150 meters. Concretions of the Silurian La Vieille Formation and Lower Ordovician Levis Formation started to form at somew
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Kim, Muriel. "The controls of sedimentary links on the spatial distribution of Atlantic salmon («Salmo salar») juveniles and spawning activity along rivers in the Gaspé Peninsula, Canada." Thesis, McGill University, 2009. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=40685.

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The longitudinal trend in the size of a river’s bed material is best represented as being composed of several discrete units, called sedimentary links, in which each sedimentary link is initiated by a source of coarse sediment, and the bed material becomes progressively finer in the downstream direction. In this study, the concept of sedimentary links is applied to salmon rivers in the Gaspé Peninsula of Quebec, Canada, which have previously not been studied in the context of sedimentary links. Also, the relationship between the sedimentary links and the distributions of Atlantic salmon (Salmo
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Charpentier, Alain. "Sylvain Rivière, écrivain régionaliste contemporain." Thesis, McGill University, 2004. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=82694.

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Quebec knew a long tradition of regionalistic literature since the novel of the soil, tradition with which the writers of Quebec broke for a long time. However, certain writers still practice a regionalistic form of literature, which does not have anything to see with the novel of the soil. Within the literary institution, the regionalistic writers of today seem to belong to a sphere of distinct production. In order to delimit the space occupied by the contemporary regionalistic writers, we based ourselves on the theory of the literary field of Pierre Bourdieu and the theory of the inst
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Lawrence, D. A. "Sedimentology of the Lower Devonian Battery Point Formation, Eastern Gaspe Peninsula, Quebec, Canada." Thesis, University of Bristol, 1986. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.375399.

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Books on the topic "Gaspé Peninsula"

1

Wendell, Townsend Charles. Notes on the summer birds of the Gaspé Peninsula, province of Quebec. s.n., 1997.

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2

Mimeault, Mario. L'exode québécois 1852-1925: Correspondance d'une famille dispersée en Amérique. Editions du Septentrion, 2013.

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3

Rand, Silas Tertius. Micmac place-names in the Maritime Provinces and Gaspé Peninsula recorded between 1852 and 1890. s.n.], 1996.

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4

Jules, Bélanger, ed. Almanach littéraire gaspésien. Guérin littérature, 1988.

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5

Gray, James T. Quaternary processes and paleoenvironments in the Gaspe Peninsula and the Lower St-Lawrence Valley. National Research Council of Canada, 1987.

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6

Cox, Philip. Fresh water fishes and batrachia of the peninsula of Gaspe, P.Q. and their distribution in the Maritime Provinces of Canada. s.n.], 1994.

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7

Die Balkankrise ALS Gegenstand Der Gemeinsamen Auen- Und Sicherheitspolitik (Gasp): Die Eu Zwischen Integration Und Kooperation (Europaische Hochschulschriften: Reihe 31, Politikwissenschaf). Peter Lang Publishing, 2004.

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Book chapters on the topic "Gaspé Peninsula"

1

Malo, M., B. Dubé, V. Garnier, and A. Chagnon. "Carlin-like gold mineralization in the Gaspé Peninsula, Canadian Appalachians." In Mineral Deposit Research: Meeting the Global Challenge. Springer Berlin Heidelberg, 2005. http://dx.doi.org/10.1007/3-540-27946-6_141.

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2

Germain, Daniel, Bernard Hétu, and Louise Filion. "Tree-Ring Based Reconstruction of Past Snow Avalanche Events and Risk Assessment in Northern Gaspé Peninsula (Québec, Canada)." In Advances in Global Change Research. Springer Netherlands, 2010. http://dx.doi.org/10.1007/978-90-481-8736-2_5.

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3

Malo, Michel, and Pierre-André Bourque. "Timing of the deformation events from Late Ordovician to Mid-Devonian in the Gaspé Peninsula." In Geological Society of America Special Papers. Geological Society of America, 1993. http://dx.doi.org/10.1130/spe275-p101.

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4

Bourque, Pierre-Andre. "Silurian stratigraphy and facies, Port-Daniel/Gascons and Black-Cape areas, southern Gaspé Peninsula, Québec." In Centennial Field Guide Volume 5: Northeastern Section of the Geological Society of America. Geological Society of America, 1987. http://dx.doi.org/10.1130/0-8137-5405-4.379.

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Reports on the topic "Gaspé Peninsula"

1

Pinet, N., D. Lavoie, P. Brouillette, et al. Gravity and aeromagnetic atlas of the Gaspé Peninsula. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2005. http://dx.doi.org/10.4095/221216.

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Brouillette, P., N. Pinet, P. Keating, D. Lavoie, D. J. Dion, and R. Boivin. The Gaspé Peninsula: new gravity and aeromagnetic datasets and their enhancement. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2006. http://dx.doi.org/10.4095/221960.

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Gagnon, Y. D., and R. A. Jamieson. Geology of the Mont Albert region, Gaspe Peninsula, Quebec. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1985. http://dx.doi.org/10.4095/120205.

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Doyon, M., C. Dalpe, and G. Valiquette. Silurian and Devonian Volcanic Rocks of the Gaspe Peninsula. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1990. http://dx.doi.org/10.4095/130886.

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Laurent, R., and J. Dostal. The Siluro - Devonian Basalt - Holeiitic Andesite Association From the Gaspe Peninsula. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1990. http://dx.doi.org/10.4095/130888.

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Hesse, R., and E. Dalton. Diagenetic - Low Grade Metamorphic Trends in the Acadian Belt of Gaspe - Peninsula. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1990. http://dx.doi.org/10.4095/130871.

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7

Bolton, T. E. Early Silurian Bryozoa From the Clemville Formation of the Port Daniel Region, Gaspe Peninsula, Quebec. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1986. http://dx.doi.org/10.4095/120634.

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8

Stevens, K. Continuation of a Metallogenic / Exploration Study For Granite - Associated Mineralized Regions in the Gaspe Peninsula, Quebec. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1989. http://dx.doi.org/10.4095/130736.

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