Transect of the southwestern Grenville Province / A. Davidson [and others]

by Davidson, A.

Publisher: Geological Association of Canada in Saskatoon

Written in English
Published: Pages: 114 Downloads: 272
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  • Geology - Ontario - Grenville Province

Edition Notes

SeriesGAC/MAC 2002. Field trip guidebook B6
ContributionsEaston, R.M.
The Physical Object
Pagination114 p. + 2 plates
Number of Pages114
ID Numbers
Open LibraryOL22068407M

Full text of "Journals of the Legislative Assembly of the Province of Ontario" See other formats Grenville Province is thicker (39 km) than the Superior Province (35 km) (Berry and Fuchs, ). Seismic wave velocities in the upper Grenville crust are = kmls faster than in the Superior Province suggesting that crust in the Grenville Province is denser. Two seismic profiles crossing the Superior/ Mccaffery: Contemporary Issues in Pain Management, Tape One Mccaffery Thinking about Child Language - Research to Practice, Judith R. Johnston A Bibliographic Guide to the Comparative Study of Ethics, John Carman, Mark Jurgensmeyer Abran Paso a Los Patitos (Make Way for Backbone of the Americas: Shallow Subduction, Plateau Uplift, and Ridge and Terrane Collision (Geological Society of America Memoir ) | Suzanne Mahlburg Kay, Victor A. Ramos, William R. Dickinson | download | B–OK. Download books for free. Find books

Transect of the southwestern Grenville Province / A. Davidson [and others] by Davidson, A. Download PDF EPUB FB2

Davidson, A.,‘Regional synthesis of the Grenville Province of Ontario and western Quebec. Part I: Some observations on the Grenville Front, and on metamorphism and plutonic rocks in the southwestern Grenville Province’; Can., Geol.

Surv., Paper B, p. – Google Scholar Beyond North America, the Grenville Province has been recognized inside exhumed anticlinal inliers in the Caledonia of Northern Ireland, Scotland, and then in Norway and the Sveconorwegian Province in Scandinavia (Davidson, ; Lorenz et al., ).According to several authors, it would continue from Central America to Antarctica, and from India to Australia (e.g.

Karlstrom et al., ) Get this from a library. From front to interior: an Ontario transect of the Grenville province, Sudbury to the St. Lawrence. [A Davidson; R M Easton] The Grenville orogenic cycle, between ∼ and Ma, involved accretion of magmatic arcs and/or continental terranes to the Laurentian craton.

A transect across the western Central Gneiss Belt, J WF Ketchum, A Davidson, Crustal architecture and tectonic assembly of the Central Gneiss Belt, southwestern Grenville Province, Canada: a new interpretation, Canadian Journal of Earth Sciences, /e, 37,(), ().

Ketchum, JWF and Davidson, A () Crustal architecture and tectonic assembly of the Central Gneiss Belt, southwestern Grenville Province, Canada: a new interpretation.

Canadian Journal of   Davidson,for a detailed overview). In the central and southwestern Grenville Province (Fig.2),the allochthonous terranes consist mainly of the Central Metasedimentary Belt and the Central Granulite Terrane (Wynne-Edwards, ).

Except for minor intrusions and dikes, magmatism ofanmerca/uploads/8/3/4/8//corrigan___hanmer_geology_pdf. infrastructure (CGB) in the southwestern Grenville Province along normal‐sense shear zones. Box shows approximate location of study area in the CGB.

(From Schwerdtner et al. ; modified from Rivers ). A conceptual model to explain the present architecture of the Grenville Province was proposed by Rivers (,   Figure 2. Transect of oxygen isotopes of Ga A-type granitoids in the southern Grenville Province (Peck et al., ).

High 18O plutons are restricted to the Frontenac terrane, except for the Edwardsville Pluton (EP), which is adjacent to the Black Lake shear zone (on the eastern side).

MSZ= Maberly shear zone, BLSZ= Proterozoic subduction and terrane in the southwestern Grenville province, Canada: evidence from ultrapotassic to shoshonitic plutonism; Geology, Vol. 15, p. Corriveau L. Lithotectonic studies in the Central Metasedimentary Belt of the southwestern Grenville Province: plutonic assemblages as indicators of tectonic :// The Grenville Province is a classic example of an exhumed orogen, exposing the Mesoproterozoic middle crust of the margin of Laurentia ().Research in the Grenville Province has focused on using it as a natural laboratory to investigate geologic questions such as the petrology of abundant yet enigmatic anorthosite plutons, the relationship between anorthosite emplacement and regional A seismic-based cross-section of the Grenville Orogen in southern Ontario and western Quebec1 D.J.

White, D.A. Forsyth, I. Asudeh, S.D. Carr, H. Wu, R.M. Easton, and    Ketchum, J.W.F. and A. Davidson, Crustal architecture and tectonic assembly of the Central Gneiss Belt, southwestern Grenville Province, Canada - a new interpretation.

Canadian Journal of Earth Sciences - LITHOPROBE Abitibi-Grenville Special Issue, accepted. ~litho/ Davidson and L. Nadeau,‘Structural subdivisions of the Grenville Province in the Parry Sound-Algonquin region, Ontario.’ In: Current Research, Part B, Geological Survey of Canada Paper, no.

83–1B,   An alternative position for this terrane boundary is the Black Lake Shear Zone (BLSZ), which is interpreted to separate the Frontenac Terrane from the Adirondack Lowlands Terrane in the southwestern Grenville Province ().The presence of the BLSZ has previously been interpreted based on changes in the lithologic (Davidson, ) and isotopic character (Peck et al., ) between the two Systematic mapping of a transect along the well‐exposed shores of Georgian Bay, Ontario, combined with the preliminary results of structural analysis, geochronology and metamorphic petrology, places some constraints on the geological setting of high‐grade metamorphism in this part of the Central Gneiss Belt.

Correlations within and between map units (gneiss associations) have allowed us to   within this part of the Grenville orogen. Geological Setting The study area includes three major geological units: Huron Supergroup rocks of the Southern Province, felsic volcanic and high-level plutonic rocks of the Killarney Complex, and granitoid or-thogneisses, amphibolites, and paragneisses of the Grenville Front Tectonic Zone (figure 2).

The,;sequence=1. The Allochthon Boundary Thrust (ABT) is one of the most important tectonic boundaries in the Grenville Province because it defines the northwesterly limit of major terrane displacement during the – Ottawan phase of the Grenville Orogenic Cycle (Rivers et al., ).Hence it separates parautochthonous crust to the northwest from allochthonous nappes and thrust sheets to the Mesoproterozoic magnesite deposits are found associated with dolomitic marble and intercalated with metasedimentary rocks of the Grenville Supergroup in the granulite facies Morin terrane (Grenville Province, Quebec).

This study examines one of the remaining ore deposits exposed on the surface (at the Dobbie mine), and presents stable isotope and mineralogical data for a marine evaporitic :// Special offer price £43 (usual price £ / GSA&GSL £) GSA Memoir The geological evolution of the Grenville orogenic belt represents one of the most widespread episodes of crustal modification in Earth’s history.

The 39 papers in this volume offer a system-wide perspective on rocks and processes of the Mesoproterozoic Grenville orogen and Appalachian inliers and include many The Grenville Province is separated from older units such as the Superior and Southern provinces, the Killarney Magmatic Belt, the Eastern Granite-Rhyolite province and the Midcontinent Rift by the Grenville Front (GF; Williams et al).

Transect across the northwestern Grenville orogen, Georgian Bay, Ontario: Polystage convergence and extension in the lower orogenic crust: Tecton The Grenville Province presents an intermediate picture, with some crustal thickness variation, and near-uniform values of Vp/Vs and Moho thickness (Figs.

15 and 16). Of the three tectonic domains in the region, the Grenville Province has the thickest crust. Vp/Vs ratios are systematically higher than in the Superior :// Nearly all businesses, including gyms, movie theatres and indoor dining, can reopen on Friday in parts of Ontario, except for the Toronto-area and a few other regions, as the province enters Stage   The Young-Davidson Property is located within the southwestern part of the Abitibi Greenstone Belt, which is the largest preserved Archean greenstone belt in the world and one of the most continuous units of the Superior Geologic Province.

The Abitibi Greenstone Belt Over new Nd isotope analyses for the central Grenville Province in the Parent-Clova region of Quebec help fill a major gap in understanding the crustal accretion history of the province.

Nd model ages show that the Parent-Clova region consists of three crustal blocks: the Archean parautochthon in the north; a central block with mixed ages interpreted as an ensialic arc; and a southerly Western Grenville Province holds key to midcontinental Granite‐Rhyolite Province enigma Western Grenville Province holds key to midcontinental Granite‐Rhyolite Province enigma Slagstad, T.; Culshaw, N.

G.; Daly, J. S.; Jamieson, R. Introduction Formation of the eastern and southern Granite‐Rhyolite Province (Fig. 1) at c. and Ma, respectively ISBN: OCLC Number: Description: ix, pages: illustrations, maps (some color) ; 29 cm. Contents: Acknowledgments --Preface --Proterozoic tectonic evolution of the Grenville orogen in North America: An introduction / Richard P.

Tollo, Louise Corriveau, James McLelland, and Mervin J. Bartholomew --Canadian Grenville Province --Cordierite-orthopyroxene The 10% Solution for a Healthy Life (blogged version of book, with reader comments and additional materials; scroll down page to see start of book), by Ray Kurzweil (HTML at ); Abominable Snowmen: Legend Come to Life (Philadelphia and New York: Chilton Co., c), by Ivan Terence Sanderson.

page images at HathiTrust; illustrated HTML with commentary at ?title=life&tmode=words. The advertiser's pocketbook; a book of reference dealing with plans, copy, management, and other details of advertising practice. (Scranton, Pa.: International Text Book Co., ), by International Correspondence Schools (page images at HathiTrust) Advertising agency operations and ?.

The Saint-Urbain and Big Island rutile-bearing ilmenite Fe-Ti oxide deposits are located in the composite km² Saint-Urbain anorthosite ( Ma, U-Pb zircon) and in the Lac Allard intrusion ( Ma, U-Pb zircon) of km² Havre-Saint Pierre anorthosite suite, respectively, in the Grenville Province of Eastern Canada.

Slow cooling rates of °C/m.y. are estimated for Search the history of over billion web pages on the ://  Metallogeny of the Nikolai large igneous province (LIP) in southern Alaska and its influence on the mineral potential of the Talkeetna Mountains J.M.

Schmidt and R.K. Rogers Library of Congress Subject Headings for this publication: Geology, Structural -- Alaska. Plate tectonics -- Alaska.

Continental margins --