1 edition of Precambrian geology, Kaminak Lake map-area, district of Keewatin found in the catalog.
Precambrian geology, Kaminak Lake map-area, district of Keewatin
Published
by Energy, Mines and Resources in Ottawa
.
Written in English
Edition Notes
11
| The Physical Object | |
|---|---|
| Pagination | 27 p. |
| Number of Pages | 27 |
| ID Numbers | |
| Open Library | OL22022695M |
The geologic formations of Michigan span more than billion years, from some of the oldest Precambrian rocks to loose, unconsolidated drift left behind by the continental ice sheets of the Pleistocene period. The following series of maps illustrates the general configuration of the geologic basement of the Great Lakes region, and of Michigan. The Penokean Mountains formerly were assigned erroneously to late Keweenawan time. The Early Precambrian rocks are divided into the Ontarian and the Timiskamian systems. The Ontarian rocks include the Keewatin group of Minnesota and the Coutchiching metasediments which underlie the Keewatin greenstones in Ontario.
Two major areas typify District geology. The uppermost area, called the surficial geologic zone, contains materials deposited by glaciers. Precambrian, Cambrian and Ordovician rock formations make up the lower or bedrock geology. This section describes each major geologic area. Glaciers crafted the watershed's surface geology when they retreated and dropped "drift" on the land. The glacial. Although the latest comprehensive report is that of Butler and Burbank (), much of the more recent literature is covered in a review of the Keweenawan geology of the Lake Superior region by Halls () and in papers on the geology of the Michigan copper district by White (, ).
The Lower Precambrian rocks in Cook County are the eastern extension of the Vermilion district, a typical Archean metavolcanic-metasedimentary terrane. The district, as defined originally by Clements (), consti tutes a narrow belt of rocks that extends from the vicinity of Tower, near. Turek, A., and Robinson, R.N. () Geology and age of the Precambrian basement in the Windsor, Chatham, and Sarnia area, southwestern Ontario: Canadian Journal of Earth Scien – CrossRef Google Scholar.
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Get this from a library. Precambrian geology, Kaminak Lake map-area, District of Keewatin (55 L). [A Davidson]. Get this from a library. Geology of Woodburn Lake map area, District of Keewatin. [J A Fraser; Geological Survey of Canada.] -- Description of the Precambrian (Archean to Aphebian) geology of the area around Woodburn Lake, central Keewatin, Northwest Territories, drained by the Quoich and Meadowbank Rivers.
Precambrian - Precambrian - Precambrian geology: By international agreement, Precambrian time is divided into the Archean Eon (occurring between roughly billion years ago and billion years ago) and Proterozoic Eon (occurring between billion and million years ago).
After the Precambrian, geologic time intervals are commonly subdivided on the basis of the fossil record. Davidson, A. a: Precambrian geology, Kaminak Lake map-area, District of Keewatin; Geological Survey of Canada, Paper Spi Lake area, District of Keewatin. PDF | On Jan 1,S.
Hanmer and others published Geology of Kaminak greenstone belt from Padlei to Quartzite Lake, Kivalliq Region, Northwest Territories.
| Find, read and cite all the. Borrow it Toggle Dropdown Albert D. Cohen Management Library; Architecture/Fine Arts Library; Archives and Special Collections; Bibliothèque Alfred-Monnin (Université de Saint-Boniface).
Irwin, D.A. Mineral occurrences and preliminary geology of the Kaminak–Carr lakes area, District of Keewatin (parts of 55 L/3, 4, 5 and 6). Northwest Territories Geological Mapping Division, Map EGSscale 1: 50 Google Scholar. Location of the study areas (circles) in the Keewatin District of the Northwest Territories.
A.N. RENCZ AND G.E.M. HALL Archean Kaminak Group. Similarly, the rocks at Townsend Lake are horn- blende-rich diorite, tonalite, gabbro and amphibolites. In both areas the most recent ice flow direction appears to be southeastward.
Two mafic syenite intrusions are exposed to the south of the eastern end of Thirty-Mile Lake where they penetrate basement gneisses and rocks of the Kaminak (?) Group (LeCheminant et al., ). A hornblende--syenite in- trusion into the Dubawnt Group, outcropping on the east side of Tulemalu Lake, has also been tentatively correlated with the.
Geology of the Tebesjuak Lake map area: a progress report with notes on uranium and base metal mineralization. Geological Survey of Canada, Paper A, pp. – Google Scholar. A brief exploration of the Keewatin, Laurentian, Knife Lake, and Algoman periods. KLKA, for short. Early Precambrian Geology of Michigan Geo Logic Precambrian.
The Precambrian rocks, older than 2, m.y., in the Saganaga Lake-Northern Light Lake area on the Minnesota-Ontario boundary include a thick succession of metavolcanic rocks, chiefly greenstone but with some intermediate to silicic types, and minor metasediments; the Northern Light Gneiss; the Saganaga Tonalite; alkalic syenodiorite and granodiorite; and the Knife Lake Group.
Tavani map-area, situated on the west side of Hudson Bay, is in the Churchill Structural Province. Metamorphosed volcanic and sedimentary rocks of the Kaminak Group, and intrusive plutons are well exposed in the southern half of the area, and in the Rankin Inlet area.
P / Ridler, R. and Shilts, W. / EXPLORATION FOR ARCHEAN POLYMETALLIC SULPHIDE DEPOSITS IN PERMAFROST TERRAINS: An Integrated Geological/Geochemical Technique; Kaminak Lake Area, District of Keewatin, Ottawa,33 pages, 3 tables (in pocket), 25 figs.
(10 in pocket), - 3 - $ 30 Northwest Territories Miscellaneous Maps. Drift prospecting for gold in the Kaminak Lake–Turquetil Lake area, District of Keewatin; in D.G. Richardson and M. Irving, Project summaries: Canada–Northwest Territories Mineral Development Subsidiary Agreement Geological Survey of Canada, Open File ologist's office and the Mining Recorder's office nearest the map-area.
Issued Information from this publication may be quoted if credit is given. It is recommended that reference be made in the following form: Culshaw. N.G: Precambrian Geology of the Drag Lake Area, Haiiburton County. GEOSCAN supports the mission of Natural Resources Canada through the timely access to information.
12 Geology and economic resources of the Larder Lake district, Ont. And adjoining portions of Pontiac Co., Que. Can G S, Memoir pp, maps () 12a Kewagama Lake map area, Pontiacand Abitibi, Que.
Can G S, Sum Rp () 13 The Cobalt series; its character and origin. SHORTER CONTRIBUTIONS TO GENERAL GEOLOGY GEOLOGY OF PRECAMBRIAN ROCKS, CENTRAL CITY DISTRICT, COLORADO By P. SIMS and D.
GABLE ABSTRACT The Central City district, one of the major metal-mining areas in the Colorado mineral belt, is in the central part of the Front Range. It lies within a terrane of Precambrian rocks.
the geology of the Durango quadrangle, have helped me in many ways. Hinderman, geologic field as sistant, worked capably during the wet summer of GEOLOGIC SEQUENCE The Precambrian rocks of the Needle Mour tains have a complex history, including two major Prwambrian tectonic events, which consisted of: 1.
This report describes the geology of the West Minnitaki Lake Area, District of Kenora. The area, comprising about 73 square miles, includes Pickerel township and lies about 15 miles southwest of the town of Sioux Lookout.
The bedrock, which is Precambrian, consists of alternating, northeast-trending belts of metavolcanic and metasedimentary rocks.GEOLOGY AND STRUCTURE OF THE PRECAMBRIAN ROCKS IN IWOROKO, ARE AND AFAO AREA, SOUTHWESTERN NIGERIA. Olusiji Samuel Ayodele Department of Geology, Ekiti State University, P.M.B.
Ado-Ekiti. Abstract: Geologic mapping of the study area revealed three dominant lithologic units namely: banded-gneiss, migmatite-gneiss and granite-gneiss.The locality Tavani (TA-vuh-nee) was a mining settlement and trading post in the Kivalliq Region of Nunavut, mes known as Tavane, it is located on western Hudson Bay's Mistake Bay, km ( mi) south of the community of Whale Cove and 97 km (60 mi) east of Kaminak Lake.
