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2 edition of Petrology of some Grenville volcanic and pelitic rocks from near Madoc, Southeastern Ontario. found in the catalog.

Petrology of some Grenville volcanic and pelitic rocks from near Madoc, Southeastern Ontario.

Geoffrey Alexander Sampson

Petrology of some Grenville volcanic and pelitic rocks from near Madoc, Southeastern Ontario.

by Geoffrey Alexander Sampson

  • 208 Want to read
  • 9 Currently reading

Published in [Toronto] .
Written in English

    Subjects:
  • Clay.,
  • Petrology -- Ontario -- Madoc,
  • Rocks, Igneous.

  • Edition Notes

    ContributionsToronto, Ont. University.
    The Physical Object
    Paginationxiv, 218 leaves.
    Number of Pages218
    ID Numbers
    Open LibraryOL20173818M

    Many gold-arsenopyrite-sulphosalt occur- rences are hosted in carbonate rocks or thin pelitic layers in volcanic rocks. This may be a function of focussing of structure in the more ductile lithologies instead of the volcanic rocks, which seem to be a preferred host for many gold deposits elsewhere. Grenville Province, southeastern Ontario Cited by: Paleozoic geology of the Brockville-Mallorytown area, southern Ontario; Ontario Geological Survey, Preliminary Map P, scale Use and Reproduction of Content: The Content may be used and reproduced only in accordance with.

    Nunes, P.D. and Pyke, D. Time-stratigraphic correlation of the Kidd Creek orebody with volcanic rocks south of Timmins, Ontario, as inferred from zircon U-Pb ages. Economic Geology (1 Publication) Nunes, P.D. and Thurston, P.C. High-grade metamorphism in the Chapleau-Foleyet Area, Ontario JouN A. Pencrver Geological Survey of Canada Booth Street, Ottawa, Ontario KIA 0M Canada Abstract High-grade Archean rocks are exposed in the central Superior Province ofthe Canadian Shield in the Kapuskasing StructuralZone, a partly fault-bounded region up to 50 x Size: 2MB.

    The Grenville dike swarm is a large Proterozoic dike swarm in the Canadian provinces of Ontario and is one of the several major magmatic events in the Canadian Shield and it possibly formed million years ago along a triple junction that might have been related to a mantle plume. The maximum length of the Grenville dike swarm is km ( mi). O 18 /O 16 ratios have been obtained for rocks and minerals along a mile traverse from near the Grenville front north of Lake Nipissing to the Paleozoic contact to the east of Georgian Bay. Two types of oxygen isotopic relationships correlated with metamorphic grade and style of plutonic emplacement are observed: (A) from the Grenville fron to the Haliburton Highlands, upper amphibolite to Cited by:


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Petrology of some Grenville volcanic and pelitic rocks from near Madoc, Southeastern Ontario by Geoffrey Alexander Sampson Download PDF EPUB FB2

Chemical Petrology of Some Grenville Schists near Fenlight, Ontario: University of Ottawa: Regional: Petrology of the Deloro Pluton and Association Country Rocks near Madoc, Ontario: University of Toronto: Regional: Petrology of Some Grenville Volcanic and Pelitic Rocks from near Madoc, Southeastern Ontario: The rocks studied in southeastern Ontario were deposited or emplaced between and m.y.

ago and were not derived from an ancient sialic basement such as that found north of the Grenville. Petrology of the nepheline and corundum rocks of southeastern Ontario Louis Moyd. Louis Moyd and mineralizers. As the Grenville rocks were traversed by these emanations, silicates were developed in some of the dolomitic marble, and some of the basic dark gneisses were converted to syenite-like gneisses.

lost less silica to the country Cited by: The Precambrian Loon Lake pluton, Ontario, is a circular zoned body emplaced in metamorphosed rocks of the Grenville Province about ±75 m.y. : Jaroslav Dostal.

The Ontario Geological Survey has issued a Guidebook on the Rocks of the Grenville Province near Renfrew, Ontario (OFR); and a Report on the Chenaux gabbro intrusion near Renfrew (OFR) I don’t often venture up the Ottawa valley to the Town of Renfrew or to Renfrew County, as there is so much to explore in Lanark County, southern Author: Christopher Brett.

Preliminary report on the relationship of mineral deposits to intrusive rocks and metamorphism in part of the Grenville Province of southeastern Ontario.

Ontario Dept. Mines, Prelim. The Grenville Province: Up Close The making of the Grenville Province is the third stage in the formation of Ontario. Built from about billion to about billion years ago, it is the youngest part of the Canadian Shield. The rocks of the Grenville Province were baked, squeezed, stretched and twisted into metamoiphic.

and geochemical analysis (including whole rock and rare-earth element analyses) of these three units has been carried out. Results indicate that the batholith was formed by partial fusion of sedimentary and volcanic material; the homogeneous diatexite arose in a similar way although fusion was lessAuthor: Randall T.

Gillespie. A Study of Some Post-Cambrian Dike Rocks in Southeastern Ontario: Carleton University: B. T Chemical Petrology of Some Grenville Schists near Fernleigh, Ontario: Carleton University: M.

T Petrology of the Deloro Pluton and Associated Country Rocks, near Madoc, Ontario: University of Toronto: M. The Grenville orogeny was a long-lived Mesoproterozoic mountain-building event associated with the assembly of the supercontinent record is a prominent orogenic belt which spans a significant portion of the North American continent, from Labrador to Mexico, as well as to Scotland.

Grenville orogenic crust of mid-late Mesoproterozoic age (c. – Ma) is found worldwide, but. The aim of this paper is to describe the mineralogy and petrology of siliceous, dolomitic marbles in the Sharbot Lake domain, as exposed in the Almonte-Carleton Place area of Ontario.

Alteration of the Grenville rocks by magmatic emanations. Formation of nepheline Formation of corundum Later alterations Age relations.

Summary Bibliography. Assrnacr A speculative working-hypothesis is offered to account for the genesis of well-known nepheline- and corundum-bearing gneisses of southeastern Size: 1MB. Lumbers, S.B.: Stratigraphy, plutonism and metamorphism in the Ottawa River remnant in the Bancroft-Madoc area of the Grenville province of southeastern Ontario, Canada.

Thesis, Princeton University, New Jersey () Google ScholarCited by: The Grenville rocks themselves have quite a story.

The intense heat and pressure generated from the collision produced volcanic material, injected hot molten rock into the crust, and metamorphosed the sediments that had eroded from the margin of the Precambrian shield before the collision occurred. The Archean volcanic rocks and associated sedimentary rocks are intruded and deformed by two large plutons and a few smaller hypabyssal intrusions.

A petrographic and geochemical study of the Precambrian rocks exposed 1n the study area was undertaken in order to investigate the metamorphic grade and geochemical characteristics of the : Mehran.

Tabatabai. Metamorphic petrology and gravity studies of the Archean English River subprovince, western Superior Province, Manitoba and Ontario, Canada Moira E. Campion University of North Dakota Follow this and additional works at: Part of theGeology CommonsAuthor: Moira E.

Campion. The Ontario Geological Survey has issued a Guidebook on the Rocks of the Grenville Province near Renfrew, Ontario (OFR); and a Report on the Chenaux gabbro intrusion near Renfrew (OFR) I don’t often venture up the Ottawa valley to the Town of Renfrew or to Renfrew County, as there is so much to explore in Lanark County, southern.

ore petrology and. wallrock alteration studies. at the. lake shore gold mine, kirkland lake, ontario. brent ian mcinnes. a thesis submitted as partial fulfillment for the honours bachelor of science degree.

faculty of science mcmaster university hamilton, ontario. april, Author: Brent Ian McInnes. The Grenville Group of marbles, pelitic rocks and metavolcanics dating from – Ma ago occupies part of the southern Grenville Province.

It includes some of the few rocks that did not reach at least amphibolite facies of by: 7. boundary between the Precambrian rocks to the north and the Palaeozoic rocks to the south into two different physiographic parts.

The geo logical contact runs approximately through the southern edge of Moira Lake, a body of water some 3 miles long and l mile wide located just south of the town of Size: 1MB. Chemical Geology, 69 () Elsevier Science Publishers B.V., Amsterdam -- Printed in The Netherlands [3] GEOCHEMISTRY AND ORIGIN OF THE ORE CHIMNEY FORMATION, A TRANSPORTED PALEOREGOLITH IN THE GRENVILLE PROVINCE OF SOUTHEASTERN ONTARIO, CANADA LUC HARNOIS and JOHN M.

MOORE Department of Earth Sciences, Carleton University Cited by: the bedrock exposed at Old Rag Mountain formed in the Grenville event roughly 1 billion years ago Source: National Park Service, Shenandoah National Park Geologic Resources Inventory Report.

The oldest rock in Virginia, the Nellysford gneiss found in Nelson. The Ontario Geological Survey has issued a Guidebook on the Rocks of the Grenville Province near Renfrew, Ontario (OFR); and a Report on the Chenaux gabbro intrusion near Renfrew (OFR) I don’t often venture up the Ottawa valley to the Town of Renfrew or to Renfrew County, as there is so much to explore in Lanark County, southern.