The Fiskenaesset complex, West Greenland

Cover of: The Fiskenaesset complex, West Greenland |

Published by C.A. Reitzels Forlag in København .

Written in English

Read online

Places:

  • Greenland,
  • Fiskenaesset region.

Subjects:

  • Intrusions (Geology) -- Greenland -- Fiskenaesset region.,
  • Petrology -- Greenland -- Fiskenaesset region.

Edition Notes

Book details

Statementby B. F. Windley [et al.].
SeriesBulletin / Grønlands geologiske undersøgelse ;, no. 106, 108, 124, 137, pt. 1-2 also in series: Meddelelser om Grønland ;, bd. 196, nr. 2, 4, Bulletin (Grønlands geologiske undersøgelse) ;, no. 106, etc., Meddelelser om Grønland ;, bd. 196, nr. 2, etc.
ContributionsWindley, B. F.
Classifications
LC ClassificationsQ115 .D39 bd. 196, nr. 2, etc., QE611.5.G74 .D39 bd. 196, nr. 2, etc.
The Physical Object
Pagination4 v. :
ID Numbers
Open LibraryOL5114348M
ISBN 108742100887
LC Control Number74187079

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Stratigraphy and structure of the Fiskenaesset Complex, southern west Greenland (Bulletin / GrÃ, nland geologiske undersÃ, gelse) [Myers, John S] on *FREE* shipping on qualifying offers. Stratigraphy and structure of the Fiskenaesset Complex, southern west Greenland (Bulletin / GrÃ, nland geologiske undersÃAuthor: John S Myers.

The Fiskenaesset complex, West Greenland. [B F Windley;] Home. WorldCat Home About WorldCat Help. Search. Search for Library Items Search for Lists Search for Book: All Authors / Contributors: B F Windley. Find more information about: ISBN: OCLC Number: The Fiskenaesset complex, West Greenland.

[B F Windley; R K Herd; A A Bowden] Home. WorldCat Home About WorldCat Help. Search. Search for Library Items Search for Lists Search for Contacts Search for a Library. Create lists. The Fiskenaesset Complex, West Greenland, Part 1 A on *FREE* shipping on qualifying cturer: Gronlands Geologiske Undersogelse.

Book Chapter Chromitites from the Fiskenæsset anorthositic complex, West Greenland: clues to late Archaean mantle The Fiskenaesset complex Author(s) Hugh Rollinson Hugh Rollinson 1. School of Science, University of Derby, Kedleston Road, Derby DE22 1GB, UK. Search for other works by this author on.

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Bishop. Buy The Fiskenaesset Complex, West Greenland, Part II, General mineral chemistry from Qeqertarssuatsiaq (The Fiskenaesset complex, West Greenland) by Windley, Brian F (ISBN: ) from Amazon's Book Store. Everyday low prices and free delivery on eligible : Brian F Windley. Buy A preliminary study of the stratigraphy, petrology, and whole rock chemistry from Qeqertarssuatsiaq, (The Fiskenaesset complex, West Greenland) by Windley, B.

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Part I: A Preliminary Study of the Stratigraphy, Petrology, and Whole Rock Chemistry from Qeqertarssuatsiaq. Part II: General Mineral Chemistry from Qeqertarssuatsiaq. Bulletin No. and 2 Volumes.: 1st printing. 80;54pp. Octavo. Illustrated with photos, tables and graphs (including 2 plates in pocket at rear of part I).

: The Fiskenaesset complex, West Greenland, (Bulletin / Grønlands geologiske undersøgelse) () and a great selection of similar New, Used and Collectible Books available now at great prices. The Fiskenaesset Complex, West Greenland: Grønlands Geologiske Undersøgelse BulletinPart II of this book discusses the West Greenland book of many of these initial basalt properties and how.

Trove: Find and get Australian resources. Books, images, historic newspapers, maps, archives and more. Windley, B. The Fiskenaesset complex, West Greenland, by B. Windley [et al.] C.A. Reitzels Forlag Kobenhavn Wikipedia Citation Please see Wikipedia's template documentation for further citation fields that may be required.

Buy The Fiskenaesset Complex West Greenland: Part IV: Chemistry of Suphide Minerals (Bulletin no. ) by F. C Bishop, Joseph V Smith, B. (Brian F.) Windley (ISBN:) from Amazon's Book Store. Everyday low prices and free delivery on eligible : F.

C Bishop, Joseph V Smith, B. (Brian F.) Windley. Fiskenæsset complex. The work presented here is part of an ongoing joint project between the Greenland Bureau of Min-erals and Petroleum and the Geological Survey of Denmark and Greenland (GEUS). Here we report on new radiometric ages and mineral chemistry data from anorthosites from the North Atlantic craton in southern West Greenland (Fig.

Chromitites from the Fiskenæsset anorthositic complex, West Greenland: clues to late Archaean mantle processes HUGH ROLLINSON1*, CLAIRE REID2 & BRIAN WINDLEY3 1School of Science, University of. The Fiskenaesset Complex, West Greenland, Part II, General mineral chemistry from Qeqertarssuatsiaq (The Fiskenaesset complex, West Greenland): Books - Format: Unknown Binding.

Download full text in PDF Download. Advanced. The region of Qaqat Akulerit lies 60 km. to the east of Fiskenaesset, West Greenland.

The region contains several outcrops of the Fiskenaesset anorthosite complex, an association of Archaean metamorphosed and deformed stratiform igneous rocks. Earth and Planetary Science Letters, 91 () Elsevier Science Publishers B.V., Amsterdam -Printed in The Netherlands [6] Sm-Nd age of the Fiskenaesset Anorthosite Complex, West Greenland Lewis D.

Ashwal 1, Stein B. Jacobsen 2, John S. Myers 3, Feiko Kalsbeek 4 and Steven J. Goldstein Z, ' Lunar and Planetary Institute, NASA Road One, Houston, TX (U.S.A.) 2. Geochemistry and petrogenesis of Archaean metavolcanic amphibolites from Fiskenaesset, S. Greenland. Author links open overlay panel Barry L.

Weaver 1 John Tarney Barry L. Windley, B.F. () Achaean Anorthosites A Review with the Fiskenaesset Complex, West Greenland, as a Model for Interpretation. Special Publication Geological Society. West Greenland (the Fiskenæsset complex; Fig.

52, local-ity2) hosts widespread chromite mineralisation (Ghisler ). The complex, which has a strike length of more than km and an average thickness of m, has a potential estimated at million tons of low-grade Title / Author Type Language Date / Edition Publication; 1.

Stratigraphy and structure of the Fiskenaesset Complex, southern West Greenland: 1. The Archean Fiskenaesset complex contains low concentrations of Pt, Pd, and Rh in comparison with the Stillwater Complex, Montana, but variations in these concentrations with stratigraphic height show trends related to the results of igneous differentiation, even though most of the rocks have been metamorphosed and the complex has been fragmented by granitoid intrusions and repeatedly.

Introduction. Greenland (Kalaallit Nunaat in Greenlandic) is the largest island in the world covering 2, km 2, 80% of which are occupied by an up to km thick continental ice sheet in its central part (Fig. 1).The remaining ~km 2 along the coast make up a total area similar in size to Sweden or Paraguay.

Greenland has ~ 56, habitants living in towns and settlements mainly. sedimentary rocks occurring along the upper contact of the Fiskemesset gabbro-anorthosite complex with amphibolite. KEYWORDS" boron, kornerupine, Fiskenmsset, Greenland, ion microprobe, spectrophotometry.

Introduction INJ. Lorenzent discovered the mineral kornerupine from Fisken~esset, West Greenland. Main Greenlandic Ruby Occurrences. Aappaluttoq is part of the Fiskenæsset complex, where rubies occur in ultramafic rocks that are in contact with anorthosites and leucogabbroic rocks (both aluminium-rich rocks).

The ruby forming reaction is triggered by felsic sheets intersecting these rocks that intruded c. billion years ago. This probably makes the Fiskenæsset complex rubies the.

Fiskenæsset anorthosite complex (West Greenland - WG) The Achaean Fiskenæsset anorthosite complex, with a strike length of over km, is hosted in a high-grade tonalitic gneiss basement. The complex is named after the village Fiskenæsset/Qeqer tar suat - siaat.

The floor of the intrusion has not been identified, but the roof has been. InLorenzen proposed the formula MgAI2SiO6 for his new mineral kornerupine from Fiskenæsset and did not suspect it to contain boron.

Lacroix and de Gramont () reported boron in Fiskenæsset kornerupine, while Herd () found none. New analyses (ion microprobe mass analyser and spectrophotometric) of kornerupine in three specimens from the type locality, including the specimens.

some of the known chromite resources in Greenland might be triggered and led by their interesting PGE contents. - References Appel, C. C., Appel, P.W.U. & Rollinson, H.R., Complex chromite textures reveal the history of an early Archaean layered ultramafic body in West Greenland.

Mineralogical Magazine Dec. vol. 66(6); p. West Greenland Nynke Keulen and Per Kalvig Since the late s, it has been known that pink and red corundum occur in the area near Fiskenæsset (Qeqertarsuat - siaat) in southern West Greenland.

Corundum is hosted in the Fiskenæsset complex, which is part of the Archaean base - ment of the North Atlantic Craton.

To date, c. 40 corundum. Author of The evolving continents, The Fiskenaesset Complex, West Greenland, A preliminary study of the stratigraphy, petrology, and whole rock chemistry from Qeqertarssuatsiaq, Superposed deformations of the Ketilidian gneisses in the Sardloq area, S.

Greenland, Tectonic Evolution of the Himalayas and Tibet (Royal Society Discussion Volumes), The Precambrian geology of the Sârdloq area.

Its journals, Special Publications and books are internationally renowned and are available electronically via the Society's own Lyell Collection, and also via GeoScienceWorld.

Chromitites from the Fiskenæsset anorthositic complex, West Greenland: clues to late Archaean mantle processes. Geological history of the Bjørnesund region, southern West Greenland (c.

62–63° N). • Locus of gold enrichment defined by competence contrast during shearing folding. • Gem-corundum result of reaction anorthite + ultramafic rock triggered by pegmatite.

• Connection between Fiskenæsset complex and Ravns Storø supracrustal belt. History. Ingem-quality ruby was discovered in outcrop on what became known as Ruby Island by Dr.

Martin Ghisler, with the Geological Survey of Denmark and Greenland (GEUS). Ghisler's scouts and support staff drew heavily from the knowledge of the native population of the nearby village of Qeqertarsuatsiaat (formerly Fiskenaesset).The exploration team discovered ruby in association with.

Friend, C.R.L. (): A1-Cr substitution in peraluminous sapphirines from the Bjoernesund area, Fiskenaesset region, southern West Greenland. Mineralogical Magazine. 46, ⓘ Sapphirine-occurrence NE of Bjørnesund. The geological map in scale 1: is an amalgamation of the harmonised, seamless map of southern West and South-West Greenland between 61° 30´ N and 64° N (Keulen et al.

) and additional digitised and harmonised maps of South Greenland.Flood basalt provinces in East Greenland and in West Greenland, record major magmatic activity, and cover areas of more tkm² km², respectively. Their numerous dyke and sill systems, are generally viewed as having a promising potential for nickel accumulation.Pink sapphire and ruby (corundum) have been discovered in more than 40 localities in the area near Fiskenæsset (Qeqertarsuatsiaat), southern West-Greenland.

A few localities yield stones of gem quality, especially in the area near Aappaluttoq. GEUS has investigated the pink sapphire and ruby from these localities together with MMR, Nuuk.

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