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Wednesday, April 22, 2020 | History

3 edition of Polyphase deformation in the Canadian Shield of northeastern Alberta found in the catalog.

Polyphase deformation in the Canadian Shield of northeastern Alberta

C. W. Langenberg

Polyphase deformation in the Canadian Shield of northeastern Alberta

  • 29 Want to read
  • 18 Currently reading

Published by Alberta Research Council in Edmonton, Alta .
Written in English

    Places:
  • Alberta.
    • Subjects:
    • Rock deformation -- Alberta.,
    • Geology, Stratigraphic -- Precambrian.,
    • Shields (Geology) -- Alberta.

    • Edition Notes

      StatementC.W. Langenberg.
      SeriesBulletin / Alberta Research Council ;, 45, Bulletin (Alberta Research Council) ;, 45.
      ContributionsAlberta Geological Survey.
      Classifications
      LC ClassificationsQ180.C2 R34 no. 45, QE604 R34 no. 45
      The Physical Object
      Pagination33 p. :
      Number of Pages33
      ID Numbers
      Open LibraryOL2902202M
      LC Control Number84130593


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Polyphase deformation in the Canadian Shield of northeastern Alberta by C. W. Langenberg Download PDF EPUB FB2

Get this from a library. Polyphase deformation in the Canadian Shield of northeastern Alberta. [C W Langenberg; Alberta Geological Survey.] -- Summarizes the structural geology of the exposed Canadian Shield of northeastern Alberta. The successive phases of deformation are put in a temporal framework, based on geochronological studies.

Request PDF | Elastic Anisotropy of a Metamorphic Rock Sample of the Canadian Shield in Northeastern Alberta | The presence of fractures and textures cause. American Libraries Canadian Libraries Universal Library Community Texts Project Gutenberg Biodiversity Heritage Library Children's Library.

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Full text of "Publications list". Initial seismic observations from a deep borehole drilled into the Canadian Shield in northeast Alberta Article (PDF Available) in International Journal of Earth Sciences (6).

This age range suggests derivation mainly from the nearby Canadian shield or Wyoming province (Gehrels and Pecha, ). The Wopmay orogen, which represents accretion of Proterozoic crust along the west flank of the Archean Slave Province (Ross,) ca. Ga (Hildebrand et al., ) (Fig. 12), is a likely source of detrital Cited by: 3.

Glacitectonics can be defined as “the deformation caused as a glacier or ice sheet pushes into and overrides a pre-existing sequence of sediments and/or bedrock” (Banham,Croot,Meer,Aber et al.,Aber and Ber,Phillips et al., ).This deformation typically involves folding and thrusting (), and therefore results in a similar range of structures to those.

Unfortunately, this book can't be printed from the OpenBook. If you need to print pages from this book, we recommend downloading it as a PDF. Visit to get more information about this book, to buy it in print, or to download it as a free PDF.

ELSEVIER Precambrian Research 91 () Prernmbrinn Resenrth Archean magmatism and deformation were not products of plate tectonics Warren B.

Hamilton * Department of Geophysics, Colorado School of Mines, Golden, C, USA Received 4 October ; accepted 30 June Abstract The granite-and-greenstone terrains that Cited by:   Manhica ADST, Grantham GH, Armstrong RA, Guise PG, Kruger FJ () Polyphase deformation and metamorphism at the Kalahari Craton-Mozambique Belt boundary.

In: Miller JA, Holdsworth RE, Buick IS, Hand M (eds) Continental reactivation and reworking. Special Publications, vol Geological Society of London, London, pp – Google ScholarCited by: 3.

Abstract Detailed geologic mapping and new SHRIMP (sensitive high-resolution ion microprobe) U-Pb zircon, Ar/Ar, Lu-Hf, 14 C, luminescence (optically stimulated), thermochronology (fission-track), and palynology reveal the complex Mesoproterozoic to Quaternary geology along the ~ km length of the Blue Ridge Parkway in Virginia.

American Libraries Canadian Polyphase deformation in the Canadian Shield of northeastern Alberta book Universal Library Community Texts Project Gutenberg Biodiversity Heritage Library Children's Library.

Open Library. Community Audio. Featured movies All video latest This Just In Prelinger Archives Democracy Now. Full text of "Research report". Summary. Following the discovery of significant thicknesses of oxidized and primary volcanogenic massive sulphide (VMS) precious and base metal mineralization at Bisha during a reconnaissance diamond drilling program in lateNevsun Resources (Eritrea) Ltd mounted a major exploration effort in early to further define the mineralization at Bisha and this.

Precambrian Geology of Northeastern Alberta: Pana, Dinu: The Waugh Lake-Tazin River Network of Retrogressive Shear Zones at the Eastern Margin of the Taltson Magmatic Zone: Parent, Adeline*; Michel Malo, Muriel Thibaut: 3D Modeling the Gaspé Belt Basin Deformation: Palinspastic Restoration, Kinematics and HC Fluid Flow.

Abstract. In Chap. 2 we discussed the hydrology of evaporite depositional and early diagenetic (eogenetic) settings, in this chapter we consider diagenetic evolution in subsequent hydrological stages in a sedimentary system containing thick salt, that is, rock-fluid interactions in an evaporite-entraining sequence experiencing ongoing burial, followed by possible uplift (mesogenesis Author: John K.

Warren. albers (1 j alberta (2) (3)alcoa (2) (3), , alcoasee also aluminum aldborough aerogenerator (2)aleutian islands (1) algeria (b).

Carbonate till as a soft bed for Pleistocene ice streams on the Canadian Shield north of Lake Superior. Canadian Journal Earth Scien p. Hiemstra, J.F., Evans, D.J.A. and Ó Cofaigh, C. GEOSCAN RSS feed for GEM2: Geo-mapping for Energy and Minerals publications40Ar/39Ar hornblende and biotite cooling ages for metaplutonic rocks of.

The Ti analogue of lakargiite and Ca analogue of barioperovskite and geikielite; not analogous to tausonite (different structure). The crystal structure is parent to many important synthetic compounds.

The general formula is ABX 3, in which [12] A = larger atoms (cubooctahedral coordination), [6] B = smaller atoms (e.g., Wenk & Bulakh, ). The Sheahan Diamond Literature Reference Compilation; The Sheahan Diamond Literature Reference Compilation is compiled by Patricia Sheahan.

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institute on lake superior geology 55th annual meeting mayely, minnesota organized by: the precambrian research center university of minnesota duluth james d. miller, jr., george j. hudak, and dean m. peterson co-chairs proceedings volume 55 part 1 – program and abstracts.

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More Info: COSTEL: Technology and the Social Experience: An introduction to and a critique of the social milieu of modern Western More Info: FRENFL. 3-D geologic modeling in the Flin Flon Mining District, Trans-Hudson Orogen, Canada: evidence for polyphase imbrication of the Flin Flon - Callinan olcanogenic massive sulfide ore system White, D J; Malinowski, M; Devine, C; Gilmore, K; Schetselaar, E; Pehrsson, S.

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Recent advances in the geology of granite-related mineral deposits: The Canadian Institute of Mining and Metallurgy Special Volu p. Drexler, J.W., and Noble, D.C.,Highly oxidized sulfer-rich dacite-rhyolite magmas of the Julcani silver district, Peru: Insight into a “productive” magmatic system: Geological Society of.

The deformation found in this carbonatite was probably developed in late-magmatic conditions, guided by tectonics associated with horizontal movements in shear zones.

Thus, this work suggests that this carbonatite was the product of the reactivation of mantle sources, within a post-collision magmatic context of the Sul-Riograndense Shield.

The Perovskite Subgroup is a subgroup of the Stoichiometric Perovskites in the Perovskite are defined as oxide single perovskites. Members of this group is characterized by oxygen as the dominant anion (Mitchell et al.

NB: The Perovskite Subgroup is not to be confused with Perovskite Supergroup, to which is belongs; the latter contains all structurally. Pole list. The following list incorporates all paleomagnetic poles in the database.

You may click the appropriate pole to find additional information on its properties, and you may also compare two or more poles at the same time by clicking their links consecutively. If of Avalonia and its docking with Baltica) and the carbon cycle (e.g., high the combined Canadian ice sheets had the same effect, we should have had ~ organic carbon burial with a lowering of the p CO2).

M6 events occurring near the ice margin of the day, i.e. a rate 5 times higher than the postglacial rate. None have been confirmed as yet. Numen Book Series: Studies in the History of Religions, Volume XCIX., E.

Thomas Lawson, Timothy Light, Brian C. Wilson The Right of Life in Japan, Noel Williams Plant Engineers and Managers Guide to Energy Conservation, Albert. Thumann. Though consisting of A-type granitoids and alkaline rocks, the complex is not anorogenic but marks the end of deformation in the polyphase Eden Deformation Zone (Mumin and Corriveau, ).

The spatial association of the Bayan Obo deposit with carbonatite dykes makes the Eden Lake deposit very prospective for IOCG mineralization, but currently 5/5(1).

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References Curiale, J., Morelos, J., Lambiase, J., Mueller, W., Brunei DarussalamFile Size: 7MB. Proceedings of the 16th International Congress of Speleology, Czech Republic, Brno, JulyVolume 3 Alternate Title International Congress of Speleology ICS Proceedings Aggregation Karst Information Portal Ticklers ISSUE: K/ HAS [0] INTERNAL LINKS.

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The most abundant Archean rocks correspond to granites and gneisses. An aproximate ratio among the different igneous Archean rocks could be that considered by Goodwin () for the Canadian Shield: % of granitic rocks (gneisses and granites).

% of metacrustal rocks. % of basic-ultrabasic rocks. SA31C Abstract Title: Auroral Spatial Structures Probe Sub-Orbital Mission Preliminary Results, SA44A Abstract Title: Deformation of Polar Cap Patches During Substorms, SM12B Abstract Title: Winds and Ion Drifts Measured in the Thermospheric Footprint of Earth's Northern Magnetic Cusp During the C-REX Sounding Rocket Mission, SM51D.

Crustal evolution of the Saykhandulaan inlier, Mongolia: implications for Palaeozoic arc magmatism, polyphase deformation and terrane accretion in the southeast Gobi mineral belt.

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ISSN X () [Refereed Article] Ferguson, MRM and Ehrig, K and Meffre, S and Cherry, AR, Associations between zircon and Fe-Ti oxides in .tectonic deformation.

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