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Добірка наукової літератури з теми "Schiste de (Canada)"

Автор: Grafiati
Опубліковано: 25 липня 2024
Оновлено: 31 липня 2025

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Статті в журналах з теми "Schiste de (Canada)"

1

Petrie, Meredith Blair, Jane A. Gilotti, William C. McClelland, Cees Van Staal, and Sierra J. Isard. "Geologic Setting of Eclogite-facies Assemblages in the St. Cyr Klippe, Yukon–Tanana Terrane, Yukon, Canada." Geoscience Canada 42, no. 3 (2015): 327. http://dx.doi.org/10.12789/geocanj.2015.42.073.

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Анотація:
The St. Cyr area near Quiet Lake hosts well preserved to variably retrogressed eclogite found as sub-metre to hundreds of metre-long lenses within quartzofeldspathic schist in south-central Yukon, Canada. The St. Cyr klippe consists of structurally imbricated, polydeformed and polymetamorphosed units of continental arc crust and ultramafic–mafic rocks. Eclogite-bearing quartzofeldspathic schist forms thrust slices in a 30 km long by 6 km wide, northwest-striking outcrop belt. The schist unit comprises metasedimentary and felsic intrusive rocks that are intercalated on the metre to tens of metr
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2

KRETZ, R. "A garnet population in Yellowknife schist, Canada." Journal of Metamorphic Geology 11, no. 1 (1993): 101–20. http://dx.doi.org/10.1111/j.1525-1314.1993.tb00134.x.

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3

Seppälä, Matti. "Rock pingos in northern Ungava Peninsula, Quebec, Canada." Canadian Journal of Earth Sciences 25, no. 4 (1988): 629–34. http://dx.doi.org/10.1139/e88-060.

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Анотація:
The author reports the first pingos found in Ungava Peninsula, Quebec. The pingos, 15–30 m high, are open-system rock pingos built of very fractured schist and hornblende gabbro. At the time of observation, water was draining out of their slopes. Peat from the top of the smaller pingo was dated at 2880 ± 100 years BP.
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4

Erdmer, Philippe, Larry Heaman, Robert A. Creaser, Robert I. Thompson, and Ken L. Daughtry. "Eocambrian granite clasts in southern British Columbia shed light on Cordilleran hinterland crust." Canadian Journal of Earth Sciences 38, no. 7 (2001): 1007–16. http://dx.doi.org/10.1139/e01-005.

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The Spa Creek assemblage is a distinctive thin pericratonic succession that crosses the Okanagan Valley in the hinterland of the southern Cordilleran Orogen in Canada. The succession was ductilely deformed and metamorphosed before deposition of overlying Triassic dark metaclastic strata. A metaconglomerate within the succession, locally composed of more than 90% biotite granite clasts, yielded five fractions of euhedral zircon that define a precise U–Pb upper intercept of 555.6 ± 2.5 Ma, inferred to be the age of a nearby pluton. Other clasts in the metaconglomerate are generally more abundant
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5

RUTHERFORD, G. K., and D. J. THACKER. "CHARACTERISTICS OF TWO MAFIC SAPROLITES AND THEIR ASSOCIATED SOIL PROFILES IN CANADA." Canadian Journal of Soil Science 68, no. 2 (1988): 223–31. http://dx.doi.org/10.4141/cjss88-022.

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Two soil profiles developed from mafic saprolites were examined at Economy Mountain, Nova Scotia and Kamloops, British Colombia. The underlying rocks, a tholeiitic basalt in Nova Scotia and a basic greenstone schist at Kamloops, were apparently transformed to predominantly smectitic saprolites in pre-Holocene times. During the Wisconsinan glacial stage the sola and a significant portion of the saprolites were removed. Holocene pedogenesis has produced new sola on the saprolites. In Nova Scotia, the solum may have some locally derived till or colluvium component. Key words: Mafic pedogenesis, P
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6

Jattiot, Romain, Nathalie Coquel-Poussy, Isabelle Kruta, Isabelle Rouget, Alison J. Rowe, and Jean-David Moreau. "The first gladius-bearing coleoid cephalopods from the lower Toarcian “Schistes Cartons” Formation of the Causses Basin (southeastern France)." PeerJ 12 (February 26, 2024): e16894. http://dx.doi.org/10.7717/peerj.16894.

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The fossil record of gladius-bearing coleoids is scarce and based only on a few localities with geological horizons particularly favourable to their preservation (the so-called Konservat-Lagerstätten), which naturally leads to strongly limited data on geographical distributions. This emphasizes the importance of every new locality providing gladius-bearing coleoids. Here, we assess for the first time the gladius-bearing coleoid taxonomic diversity within the lower Toarcian “Schistes Cartons” of the Causses Basin (southeastern France). The material includes two fragmentary gladii, identified as
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7

Minter, D. W., and P. F. Cannon. "Myriospora scabrida . [Descriptions of Fungi and Bacteria]." Descriptions of Fungi and Bacteria 227 (January 2021): 2265. http://dx.doi.org/10.1079/dfb/20210391610.

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Abstract A description is provided for Myriospora scabrida , a lichen-forming species occurring on various rock types, particularly sandstone, often but not exclusively associated with heavy metal deposits in old mine spoil heaps and on worked stone. Some information on its dispersal and transmission and conservation status is given, along with details of its geographical distribution (Tunisia, Greenland, Norway, Afghanistan, Iran, Russia, Austria, Bosnia-Hercegovina, Czech Republic, Finland, France, Germany, Iceland, Irish Republic, Italy, Norway, Russia, Spain, Sweden, Ukraine, UK, Canada (N
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8

Pan, Yuanming, Michael E. Fleet, and Neil D. Macrae. "Oriented monazite inclusions in apatite porphyroblasts from the Hemlo gold deposit, Ontario, Canada." Mineralogical Magazine 57, no. 389 (1993): 697–707. http://dx.doi.org/10.1180/minmag.1993.057.389.14.

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AbstractOriented inclusions of monazite occur in the dark core of apatite porphyroblasts in a muscovite schist from the Archaean Hemlo gold deposit, Ontario, Canada. The monazite inclusions are elongated along the b-axis and parallel to the c-axis of the apatite host; the complete orientation relationship of the monazite/apatite intergrowth is bMnz//cAp, cMnz//aAp. From analysis by SIMS and EMP, the dark core of the apatite porphyroblasts is depleted in LREE (LaN/YbN = 0.56). The monazite inclusions are correspondingly enriched in LREE, but markedly depleted in HREE, compared with monazite gra
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9

Charan, S. N., S. M. Naqvi, and S. L. Ramesh. "Geology and Geochemistry of Spinifex-Textured Peridotitic Komatiite from Mayasandra Schist Belt, Karnataka." Journal Geological Society of India 32, no. 4 (1988): 343–50. http://dx.doi.org/10.17491/jgsi/1988/320407.

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Abstract Spinifex-textured peridotitic komatiite occurs on the southeastern margin of Mayasandra schist belt near Nagamangala in Karnataka. Preservation of spinifex-texture made up of pseudomorphically altered phenocrysts of olivine and less commonly clinopyroxene set in a groundrnass of skeletal augite and devitrified glass in the komatiite, is essentially perfect in spite of alteration, deformation and metamorphism. Petrography shows dissimilar shapes and dimensions of the crystals, with more than one pattern of crystal arrangement in the texturally layered komatiite, clearly indicating that
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10

Srikantia, S. V., and S. S. Bose. "Archaean Komatiites from Banasandra Area of Kibbanahalli Arm Of Chitradurga Supracrustal Belt in Karnataka." Journal Geological Society of India 26, no. 6 (1985): 407–17. http://dx.doi.org/10.17491/jgsi/1985/260605.

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Анотація:
Abstract The Banasandra Komatiites occur within the Kibbanahalli arm of the Chitradurga supracrustal Belt in Karnataka. They apparently overlie the Bababudan Group and the Peninsular Gneiss and occur in two isolated exposures, (i) east of Birasandra, and (ii) near Kodihalli - Kunikenahalli. Ultramafic rock types include pillowed serpentinites, spinifex-textured komatiite, massive and schistose serpentinite and talc-tremolite-chlorite schist. Certain quartz-antigorite (birbirite ?), quartz-amphibole, and high-magnesian chlorite rocks are also closely associated with the ultramafics. The major e
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Дисертації з теми "Schiste de (Canada)"

1

Thorette, Jacques. "Contribution à l'étude de l'hydrothermalisme océanique : exemple du district minéralisé de York-Harbour (massif ophiolitique de Blow-Me-Down, Bay-of-Islands, Terre-Neuve)." Brest, 1986. http://www.theses.fr/1986BRES2002.

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Анотація:
Les mineralisations a cu-fe-zn de york-harbour sont encaissees dans l'unite volcanique situee au sommet de l'ophiolite cambrienne de blow-me-down. Celle-ci s'est formee a l'axe d'une dorsale oceanique a proximite d'une faille transformante. L'organisation en synclinal du secteur mineralise resulte du rejet des failles synvolcaniques en direction nord 135 et nord 45
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2

MacKenzie, Douglas James, and n/a. "Structural controls on orogenic gold mineralisation in the Otago Schist, New Zealand and the Klondike Schist, Canada." University of Otago. Department of Geology, 2008. http://adt.otago.ac.nz./public/adt-NZDU20080704.085108.

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Анотація:
Orogenic gold mineralisation in schist terranes with few or no contemporaneous igneous intrusions is poorly understood. It is proposed in this thesis that the structural evolution of such terranes controls the generation of hydrothermal fluid pathways and thus the location of orogenic mineral deposits. Gold mineralisation in the Otago Schist, New Zealand and the Klondike Schist, Canada occurred in the latter phases of greenschist facies metamorphism as well as after metamorphism during Paleozoic-Mesozoic exhumation. In Otago, gold mineralisation occurred at a number of different times and stru
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3

Girault, Michel. "Pétrographie et géochimie de volcanites archéennes polymétamorphiques : reconstitution de l'histoire pétrologique (zone minière Manitou-Louvem, Val d'Or, Québec)." Phd thesis, Grenoble 1, 1986. http://tel.archives-ouvertes.fr/tel-00739836.

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La zone Manitou-Louvem, à minéralisations de sulfures massifs, comporte une série volcanique sous-marine (laves, pyroclastites et siIls) appartenant, pour l'essentiel, à la formation de Val d'Or. A la base, des basaltes à amphiboles et boules d'épidote dérivent, par faible fusion partielle, d'une source mantellique enrichie en éléments hygromagmaphiles légers. Vient ensuite l'intime association de laves intermédiaires et felsiques, de pyroclastites grossières généralement felsiques et monogéniques, et de filon-couches hypovolcaniques de diorite. Toutes ces roches sont comagmatiques, et liées a
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4

Ramírez-Guerrero, Greta M. "The systematics and evolution of Cambrian graptolites from the Burgess Shale of Canada." Thèse, 2019. http://hdl.handle.net/1866/22745.

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Книги з теми "Schiste de (Canada)"

1

Rogers, R. Vashon. Schism: A sermon preached at Bytown before the Eastern Clerical Association, on Thursday, January 10th, 1839 and published at their request. s.n., 1987.

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2

Schreiner, Jan. Ahoi Berlin: Hauptstadt am Wasser--Bauten, Schiffe, Häfen, Brücken. Welz, 1999.

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3

Gould, Stephen Jay. Wonderful life: The Burgess Shale and the nature of history. W.W. Norton, 1989.

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4

Gould, Stephen Jay. Wonderful life: The Burgess Shale and the nature of history. Hutchinson Radius, 1990.

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5

Gould, Stephen Jay. Wonderful life: The Burgess Shale and the nature of history. W.W. Norton, 1989.

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6

Gould, Stephen Jay. Wonderful life: The Burgess shale and the nature of history. Penguin, 1991.

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7

Cotton, Matthew, Kathy Brasier, John Whitton, and Ioan M. Charnley-Parry. Governing Shale Gas: Development, Citizen Participation and Decision Making in the US, Canada, Australia and Europe. Taylor & Francis Group, 2018.

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8

Cotton, Matthew, Kathy Brasier, John Whitton, and Ioan M. Charnley-Parry. Governing Shale Gas: Development, Citizen Participation and Decision Making in the US, Canada, Australia and Europe. Taylor & Francis Group, 2018.

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9

Governing Shale Gas: Development, Citizen Participation and Decision Making in the Us, Canada, Australia and Europe. Taylor & Francis Group, 2018.

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10

Feix, Ingrid. Niederfinow: Wo die Schiffe Fahrstuhl fahren. Bebra Verlag, 2012.

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Частини книг з теми "Schiste de (Canada)"

1

Miville, Serge. "Le Grand « Schisme » ?" In Retour sur les États généraux du Canada français. Presses de l'Université du Québec, 2016. http://dx.doi.org/10.1515/9782760543829-005.

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2

"NOT AN EXOTIC VERSION OF CANADA." In Schism. MQUP, 2019. http://dx.doi.org/10.2307/j.ctvqmp1cb.10.

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3

"From Inch’Allah Dimanche to Sharia in Canada: Empire Management, Gender Representations, and Communication Strategies in the Twenty-First Century." In From Solidarity to Schisms. Brill | Rodopi, 2009. http://dx.doi.org/10.1163/9789042027039_016.

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4

"Margaret Atwood’s Oryx and Crake: Canadian Post-9/11 Worries." In From Solidarity to Schisms. Brill | Rodopi, 2009. http://dx.doi.org/10.1163/9789042027039_015.

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5

Poulsen, K. Howard, Rodney Barber, and François Robert. "Chapter 4: Hemlo Gold System, Superior Province, Canada." In Geology of the World’s Major Gold Deposits and Provinces. Society of Economic Geologists, 2020. http://dx.doi.org/10.5382/sp.23.04.

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Анотація:
Abstract Hemlo combines several rare to unique features in the spectrum of Archean greenstone gold deposits. It is an isolated, approximately 800-metric ton (t) gold system in a region of otherwise limited known gold endowment. The geology of Hemlo is dominated by deformed and metamorphosed sedimentary, felsic volcanic, and volcaniclastic units, a premineral coherent felsic porphyry, and a swarm of mainly postmineral, intermediate, feldspar-phyric dikes. Ore is dominantly in the form of gold-bearing lenses of pyritic, feldspathic schist derived from deformation of both the clastic rocks and th
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6

Schilt, Thibaut. "Denis Côté on the Road from Radisson to Locarno." In Quebec Cinema in the 21st Century. Liverpool University Press, 2024. http://dx.doi.org/10.3828/liverpool/9781802074765.003.0009.

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In this chapter, Thibaut Schilt focuses on the reception and perception of Denis Côté’s cinema in Quebec, anglophone Canada, and other parts of the world. He analyses the iconoclastic New Brunswick-born, Quebec-based auteur’s career through the lens of world film festivals, including those where the director received his most prestigious accolades: the Locarno International Film Festival and the Berlinale. After considering Côté’s cinematic output within the much discussed Renouveau du cinéma québécois (or Quebec New Wave) trend, the author continues with an overview of the various ways that C
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7

White, Chris E., Sandra M. Barr, James L. Crowley, Deanne van Rooyen, and Trevor G. MacHattie. "U-Pb zircon ages and Sm-Nd isotopic data from the Cobequid Highlands, Nova Scotia, Canada: New contributions to understanding the Neoproterozoic geologic history of Avalonia." In New Developments in the Appalachian-Caledonian- Variscan Orogen. Geological Society of America, 2022. http://dx.doi.org/10.1130/2021.2554(07).

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ABSTRACT Forty-three new U-Pb zircon ages from metasedimentary and igneous rock units throughout the Cobequid Highlands of northern mainland Nova Scotia, Canada, provide new insights into the Neoproterozoic evolution of this long-enigmatic part of Avalonia in the northern Appalachian orogen. Contrasts in ages and rock types resulted in the identification of fault-bounded Neoproterozoic assemblages of units forming the Bass River, Jeffers, and Mount Ephraim blocks. In the Bass River block, quartzite, metawacke, and minor calc-silicate rocks and marble (Gamble Brook Formation) with a maximum dep
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Тези доповідей конференцій з теми "Schiste de (Canada)"

1

Winhausen, L., K. Khaledi, M. Jalali, and F. Amann. "Insights into the Anisotropic, Hydro-Mechanical Behavior of Opalinus Clay Through Experimental and Microstructural Investigations." In 56th U.S. Rock Mechanics/Geomechanics Symposium. ARMA, 2022. http://dx.doi.org/10.56952/arma-2022-2075.

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ABSTRACT: For analyzing the influence of structural anisotropy on the hydro-mechanical behavior of a clay shale, we performed three consolidated, undrained triaxial compression tests with different geometric specimen configurations. Opalinus Clay specimens were tested with bedding plane orientations of 30°, 60°, and 90° with respect to the horizontal. Results indicated different peak strengths at failure with highest and lowest values for the 90° and 30°-specimens, respectively. Failure occurred at different mean effective stresses with different magnitudes of pore water pressure built up. The
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