Published 1975 by Dept. of Energy, Mines and Resources : available from Information Canada in Ottawa .
Written in EnglishRead online
|Statement||R. F. Emslie ; with petrographic contributions by I. F. Ermanovics.|
|Series||Paper- Geological Survey of Canada ; 74-48, Paper (Geological Survey of Canada) ;, 74-48.|
|Contributions||Ermanovics, I. F., joint author.|
|LC Classifications||QE185 .A42 no. 74-48, QE611.5.C2 .A42 no. 74-48|
|The Physical Object|
|Pagination||v, 37 p. :|
|Number of Pages||37|
|LC Control Number||76371797|
Download Major rock units of the Morin complex, southwestern Quebec
Get this from a library. Major rock units of the Morin complex, southwestern Quebec. [R F Emslie; I F Ermanovics]. Emslie has written: 'Major rock units of the Morin complex, southwestern Quebec' -- subject(s): Geology, Intrusions (Geology) 'Geology and petrology of the Harp Lake Complex, central.
Doig, R. () U-Pb zircon dates of Morin anorthosite suite rocks, Grenville Province, Quebec, Jour. Geol. 99, – CrossRef Google Scholar Drake, A.A. () The Reading Prong of New Jersey and eastern Pennsylvania: an appraisal of rock relations and chemistry of a major Proterozoic terrane in the Appalachians, in M.J.
Bartholomew, E.R Cited by: 7. Emslie RF () Major rock units of the Morin Complex, southwestern Quebec. Geol Surv Can Paper 74––37 Google Scholar Fabian K, McEnroe SA, Robinson P et al () Exchange bias identifies lamellar magnetism as the origin of the natural remanent magnetization in Cited by: 5.
The Morin terrane is located in the southwestern Grenville Province and is geologically similar to the Adirondack Highlands to the south, both having been metamorphosed to the granulite facies and hosting numerous plutons of the anorthosite-mangerite-charnockite-granite (AMCG) suite ().Because of its geology, most studies in the Morin terrane have focused on anorthosite-suite magmatism Cited by: 5.
The petrography, rock association, mineralogy, geochemistry and the problems of formation of the Ti-magnetite layers in the complex are described and discussed.
The GSC Rock-Eval Database includes samples of Utica with the following characteristics: TOC up to %, averaging %; Tmax up toaveraging ; S1 up toaveraging ; S2 up to.
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The Superior Craton is a stable crustal block (a very large block of rock) in Canada, covering Quebec, Ontario, SE Manitoba and northern Minnesota, the is the biggest craton among those formed during the Archean period.  A craton is a large part of the Earth's crust that has been stable and subjected to very little geological changes over a long time.
. Anorthosite massifs, rapakivi granites, and late proterozoic rifting of north America Nature and origin of anorthositic suites.
Geosci. Can., 2: Emslie, R.F., c. Major rock units of the Morin complex, southwestern Quebec (with petrographic contributions by I.F. Ermanovics).
R.F. EmslieMajor rock units of the Morin complex Cited by: Late-tectonic granitic pegmatites occur throughout most of the southwestern Grenville Province of Ontario and Quebec. These vary from mineralogically simple (3–4 major phases) to complex (> 4 major phases) pegmatites; the latter are variably enriched in U, Th, Mo, and rare-earth elements (REE) and Zr and by: is a city in southwestern Quebec, Canada, 40 km northwest southwestern Quebec book the city of Montreal in the regional county of Laurentides more precisely in the district of Thérèse-De Blainville.
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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.
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