2 edition of Igneous rocks of Central Labrador, with emphasis on anorthositic and related intrusions found in the catalog.
Igneous rocks of Central Labrador, with emphasis on anorthositic and related intrusions
R. F. Emslie
Part of the Field excursion guidebook series AC of the 24th International Geological Congress, Montreal, Quebec, 1972.
|Statement||R.F. Emslie, S.A. Morse, E.P.Wheeler.|
|Series||Guidebook = -- Field excursion / 24th International Geological Congress. AC -- A54|
|Contributions||Morse, S. A., Wheeler, E. P., International Geological Congress, (24th : 1972 : Montreal)|
KIGLAPAIT BIBLIOGRAPHY 13 October BOOKS The Kiglapait Layered Intrusion, Labrador. Geol. Soc. Amer. Memoir , pp. (R.F. Emslie, S.A. Morse, E.P. Wheeler) Igneous Rocks of Central Labrador, with Emphasis on Anorthosite. J. H. Regional geobarometry in the contact aureoles of the anorthositic Nain Complex, Labrador. J File Size: 83KB. The Nain Complex consists of a wide variety of rock types and intrusions, mostly anorthosite and mapped over an area of ab square kilometers. Rock types range from anorthosite, norite, leuconorite, jotunite, fayalite-bearing opdalite, leucodiorite, diorite, syenodiorite, adamellite, troctalite-syenite, farsundite, charnockite, granodiorite, granite, to alaskite.
What is magmatism? Unanswered Questions Magmatism, Petrology 'Igneous rocks of central Labrador with emphasis on anorthositic and related intrusions' -- subject(s): Geology, Guidebooks. Classification of Igneous Rocks. Igneous rocks are CLASSIFIED according to their mineral composition and texture.. Minerals form as molten rock crystallizes. A generalized order of crystallization of minerals is shown in the Bowen's Reaction the magma cools, first olivine, then pyroxene, then amphobole, etc. will be crystallized (assuming the proper elements are available).
Monzonoritic rocks (=jotunites) related to late-Proterozoic massif type anorthosites in the Rogaland province () appear (i) as fine grained dykes crosscutting the large anorthositic bodies, (ii) as chilled margins related to leuconorites-norites (Hidra, Garsaknatt, Bjerkrem-Sokndal), (iii) as separated intrusions (Eia-Rekefjord. Isotopic Data for Late Cretaceous Intrusions and Associated Altered and Mineralized Rocks in the Big Belt Mountains, Montana By Edward A. du Bray, Daniel M. Unruh, and Albert H. Hofstra Abstract The quartz monzodiorite of Mount Edith and the con-centrically zoned Cited by: 1.
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This rock is fine to medium grained and is composed of scattered megacrysts of plagioclase in a matrix of plagioclase, orthopyroxene (%), apatite (3%) plus minor amounts of clinopyroxene, orthoclase and opaque minerals.
The orthopyrox enes are granular and not subophitic in texture. accurate and detailed maps of north coastal Labrador, the first petrological understand ing of the suite of rocks encountered under the anorthosite problem in Labrador, and.
the field wisdom that allowed him not only to survive the rigors of this remote area. but also to do so with a good measure of comfort. EMSUE R. P., MORSE S. Aand WHEELER E. II () Igneous rocks of central Labrador, with emphasis on anorthosite.
XXIV International Geological Congress Guidebook A GILL J. and MURTHY V. () Distribution of K, Rb, Sr, and Ba in Nain anorthosite by: Plutonic rocks of the eastern part of the corridor comprise many nested and interfering anorthosite and monzonitic to granitic NPS intrusions, but also comprises some anorthositic rocks that may.
Is geology a good major. Magmatism, Petrology 'Igneous rocks of central Labrador with emphasis on anorthositic and related intrusions' -- subject(s): Geology, Guidebooks, Intrusions (Geology). Thermal aureoles surrounding intrusions of the Nain complex, Labrador, contain many unique or unusual mineral assemblages in aluminous gneisses and granulites, ironstones, and ultramafic rocks.
The Dunnage Melange, located in the central mobile belt of the Appalachian Orogen, in north-central Newfoundland, is host to several suites of igneous intrusions. These include mafic through felsic dikes, stocks, and batholiths ranging in age from Early Ordovician through Jurassic.
These intrusions are grouped into two complexes based on their. Ore deposits that are associated with mafic to ultramafic igneous rocks can generally be divided into those where the metals of interest are hosted in oxide minerals and those where the metals of interest are held as sulfides or are strongly associated with sulfides (e.g., PGE alloys, arsenides, bismuthinides).Cited by: 3.
Fifty-eight rock chips from fifteen samples of sedimentary rocks from the Ramah Group (∼ Ga) in northeastern Labrador, Canada, were analyzed for major and minor elements, including C and S, to elucidate weathering processes on the Earth's surface about Ga by: Igneous rocks of Central Labrador, with emphasis on anorthositic and related intrusions.
Igneous rocks of Central Labrador, with emphasis on anorthositic and related intrusions. Int. Abstract. Layered intrusions crystallize mainly from basaltic magma to form large bodies of igneous rocks that exhibit prominent layering and they preserve stunning rock records of the processes by which magma evolves in crustal magma by: Geochemical and radiogenic isotope (Sr-Nd) characteristics of Paleoproterozoic anorthositic and granitoid rocks in the Umiakoviarusek Lake region, Labrador, Canada.
February Canadian Journal. Igneous rocks that comprise the Cambrian Southern Oklahoma Aulacogen include: 1) voluminous anorthositic gabbros, 2) Fe-rich, Ti-rich, and P-rich, biotite-bearing gabbros, 3) A-type leucocratic alkali-feldspar rhyolite and granites (some with rapakivi textures, see Price et al., a), and 4) a suite of “late” diabase dikes.
Nearly all of Cited by: The metamorphic and igneous rocks of the Nain region are subdivided into more than twenty different units, at trations within troctolitic and anorthositic rocks. Some of the massive anorthositic rocks may prove to be a source of dimen- account of the rock types over a large part of central north-ern Labrador (Wheeler, This banner text can have markup.
web; books; video; audio; software; images; Toggle navigation. Labrador Geological Survey of Canada publications related to Labrador Morse, S. A., and Wheeler, E. II / IGNEOUS ROCKS OF CENTRAL LABRADOR, WITH EMPHASIS ON ANORTHOSITIC AND RELATED INTRUSIONS, IGC 24th Session Guidebook, Montreal,pb, 72 pages, - 3 - $ Grenville Province anorthosite massifs were derived from depleted mantle.
It is not clear whether massifs and related mafic intrusions throughout the Nain Province of Labrador were derived from enriched mantle, or were contaminated by early Archean (greater than Ma) silicic crustal materials, heretofore thought to be restricted to coastal Cited by: Extrusive.
an igneous rock formed on the surface of the Earth that cools quickly and has small crystals and fine grained textrure. Intrusive. an igneous rock formed on the inside of the Earth that cools slowly and has big crystals and coarse grained texture.
Magma. THE NAIN ANORTHOSITE PROJECT, LABRADOR: FIElD REPORT S. A. Morse, Editor Final Report under NSF Grants GA and GA to Franklin and Marshall College: "Evolution of Anorthosite and Related Crustal Rocks in Coastal Labrador", and "Facility for Crustal Studies in Coastal Labrador." S.
A. Morse, Principal InvestigatorFile Size: 5MB. Field observations demonstrate a close relationship between igneous intrusions and adjacent faults (Fig. 7) suggesting that magma exploits large-scale crustal weaknesses (e.g.
Sawyer ). Fractures associated with faulting may, therefore, be favourable locations for magma emplacement (Fitch ) and significant volumes of magma can migrate.Field excursion guidebook[s] - Canada - [Donald J Glass;] Igneous rocks of central Labrador, with emphasis on Anorthositic and related intrusions --[v.
55] Iron ranges of Labrador and northern Quebec --[v. 56] Appalachian structure and stratigraphy Quebec