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The Precambrian and Pleistocene geology of the Grondines map-area, Quebec.

The Grondines map-area is about twenty miles northeast of the city of Three Rivers, Quebec. Its northern and southern boundaries are latitudes 46°45' and 46°30' respectively, and its eastern and western limits are longitudes 72°00' and 72°30'. A small part of the area is south of the St. Lawrence river, which crosses the southeastern corner of the sheet. More than half the map-area is underlain by Paleozoic rocks of which the Trenton formation is the most widespread. The area of the Trenton is a little less than that of the combined area of the Black River, Lorraine, Richmond, and Queenston formation.

Identiferoai:union.ndltd.org:LACETR/oai:collectionscanada.gc.ca:QMM.109545
Date January 1953
CreatorsLunde, Magnus.
ContributorsKranck, E. (Supervisor)
PublisherMcGill University
Source SetsLibrary and Archives Canada ETDs Repository / Centre d'archives des thèses électroniques de Bibliothèque et Archives Canada
LanguageEnglish
Detected LanguageEnglish
TypeElectronic Thesis or Dissertation
Formatapplication/pdf
CoverageDoctor of Philosophy. (Department of Earth Sciences.)
RightsAll items in eScholarship@McGill are protected by copyright with all rights reserved unless otherwise indicated.
Relationalephsysno: NNNNNNNNN, Theses scanned by McGill Library.

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