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Sunday, July 12, 2020 | History

2 edition of Nunarssuit intrusive complex, South Greenland. found in the catalog.

Nunarssuit intrusive complex, South Greenland.

W. T. Harry

Nunarssuit intrusive complex, South Greenland.

by W. T. Harry

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Published by C.A. Reitzel in K©ıbenhavn .
Written in English


Edition Notes

Statementby W.T. Harry andT.C.R. Pulvertaft.
SeriesGr©ınlands Geologiske Unders©ıgelse, Meddelelser om Gr©ınland
ID Numbers
Open LibraryOL13772361M

  This granite is part of a large complex, composed predominantly of syenite, which forms the uninhabited island of Nunarssuit. The complex is the youngest in the Gardar period of rift-related alkaline magmatism, which extended from to Ma. It is generally accepted that the evolved plutons in this province formed by fractionation of The geology of Alangorssuaq, northern Nunarssuit Complex, South Greenland Author: Anderson, J. G. Awarding Body: University of Aberdeen Current Institution: University of Aberdeen Date of Award: Availability of Full Text:?uin=

Astrophyllite Group. The mineral was first found in by the Norwegian mineralogist Paul Christian Weibye () and later described by him, in , as a brown, micaous mineral ("brauner Glimmer") from Låven (formerly Lamöskjär), Langesundsfjorden, Norway (Weibye ). Later Scheerer () described it under the name :// A great range of poorly understood processes occur in magma chambers some of them leading to the development of layering. I was co-organizer, with Henning Sørensen, of a NATO Research Workshop, involving many of the best workers in the field, which was held in S Greenland in , and led to a book 'Origins of Igneous Layering' (Reidel, ), that combined both theoretical and field-based

Acknowledgements xix pioneering workers on igneous layering in Greenland xx Wbrkshop participants xxii Henning Sfl!rensen, University of Copenhagen, Dermark. Latte Melchior Larsen, Geological SUrvey of Greenland, Copenhagen, Dermark. Abstract 1 1 • Introduction 1 1. 1 The agpaitic rocks of the Igneous layering in kakortokites in the southern part of the Ilímaussaq alkaline complex, South Greenland. The central part of the photograph shows the uppermost part of the layered kakortokite series and the overlying transitional kakortokites and aegirine lujavrite on Laksefjeld ( m), the dark mountain in the left middle ground of the :// /geus-bulletin/geology-of-greenland-survey-bulletin/bulletin


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Nunarssuit intrusive complex, South Greenland by W. T. Harry Download PDF EPUB FB2

COVID Resources. Reliable information about the coronavirus (COVID) is available from the World Health Organization (current situation, international travel).Numerous and frequently-updated resource results are available from this ’s WebJunction has pulled together information and resources to assist library staff as they consider how to handle coronavirus Nunarssuit complex, Nunarssuit Island, Narsaq, Kujalleq, Greenland, Denmark: An intrusive complex, covering an area of about 45 x 25 km.

It consists of gabbros, syenites and granites, not all Buy Geology of the Western Part of the Nunarssuit Alkaline Complex, South Greenland by a.W Butterfield South Greenland.

book from Amazon's Book Store. Everyday low prices and free delivery on eligible :// Add tags for "Petrology of the Puklen syenite-alkali granite complex, Nunarssuit, South Greenland.". Be the :// The rhythmic modal layering in the Nunarssuit syenite has a vertical extent of > m and a lateral extent of >15 km.

Individual layers average 20 cm thick and grade from a relatively melanocratic The Ilímaussaq complex in South Greenland is a well-studied multiphase alkaline to peralkaline intrusion of MesoProterozoic age. Most of the Ilímaussaq rocks are extremely enriched in alkalis INTRODUCTION The Gardar Province of South Greenland comprises a mid-Proterozoic (ca.

Ma), continental intraplate and ri~-related assemblage of mildly to strongly alkaline rocks (Emeleus and Upton, ; Upton and Emeleus, ). Composition of fluid inclusions in granites and quartz syenites from the Gardar continental rift Nunarssuit intrusive complex (South Greenland). In the Puklen, the Malenefjeld, and the Helene granite belong to the Nunarssuit complex while the C.T.R.

— The Nunarssuit intrusive complex, south Greenland. Bull. Gronlands geol. Unders., 36, p. The Motzfeldt alkaline magmatic complex (MAMC) is situated on the southern tip of Greenland lying 24 km to the east of the village of Narsarsuaq (Figure 1) and km from the Atlantic coast.

The MAMC is a spectacular, glacially eroded valley occurring north east of the agpaitic intrusive units of the Ilímaussaq intrusion (Tukiainen, )   Ivigtut 61 V. 1 Syd, Nunarssuit 60 V. 1 Nord, Julianehåb 60 V. 2 Nord, Nassarssuaq 61 V. 3 Syd, Søndre Sermilik 60 V. 3 Nord, Nanortalik 60 V.

1 Syd, and Lindenow Fjord 60 Ø. 1 Nord. In the areas of South Greenland with no 1: map coverage the 1: scale map sheet Sheet 1, Sydgrønland, 2'nd edition was   The Ilímaussaq Intrusive Complex is part of the Gardar Province in South Greenland (Emeleus & Upton, ), which is interpreted to be a failed rift (Upton & Emeleus, ).

It consists of 10 major intrusions that range from alkali granite to nepheline syenite and (rare) carbonatite, along with hundreds of gabbroic to trachytic or phonolitic Acknowledgements xix pioneering workers on igneous layering in Greenland xx Wbrkshop participants xxii Henning Sfl!rensen, University of Copenhagen, Dermark.

Latte Melchior Larsen, Geological SUrvey of Greenland, Copenhagen, Dermark. Abstract 1 1 * Introduction 1 1. 1 The agpaitic rocks of the Ilimaussaq intrusion 3 2. Igneous layering in the Ilimaussaq intrusion 4 3.

Mineralogy of the layered Geology of the western part of the Nunarssuit alkaline complex, South Greenland Author: Butterfield, A. ISNI: Awarding Body: University of Aberdeen Current Institution: University of Aberdeen Date of Award: Availability of Full Text: ?uin= Abstract.

The Klokken complex in South Greenland (age + 3Ma) is a stock of layered syenite with an outer zone of rocks show sub-vertical layering and probably developed on the walls of an originally gabbroic magma chamber, which fed alkali-basaltic :// Parsons I, Butterfield AW () Sedimentary features of the Nunarssuit and Klokken syenites, South Greenland.

J Geol Soc London Brown WL, Parsons I, Becker SM () L'evolution des textures des cryptoperthites en fonction de leur position dans le succession litée de la   oval, layered gabbro-syenite intrusive complex situated at 60°56'N, 45°05'W in the Gardar igneous province of south-west Greenland.

It reaches (fig. 1) to within 1 km of the SE mar­ gin of the Igdlerfigssalik centre, the most southerly of the series of large plutons which comprise the Igaliko nepheline syenite com­ plex (Emeleus & Harry, ).

Tectonophysics, 21 (): Eisevier Scientific Publishing Company, Amsterdam - Printed in The Netherlands CRUSTAL DOWNFOLDING ASSOCIATED WITH IGNEOUS ACTIVITY D. BRIDGWATER, J. SUTTON and J.

WATTERSON The Geological Survey of Greenland, Copenhagen (Denmark} Department of Geology, Imperial College, London (Great Britain} Department of Geology, University JOURNAL OF PETROLOGY VOLUME 42 NUMBER 12 PAGES – Phase Equilibrium Constraints on Intensive Crystallization Parameters of the Ilı´maussaq Complex, South Greenland GREGOR MARKL   A' Review of the Sydprøven granite and other "New granites" of South Greenland by D.

BMDGWATER Abstract A preliminary field study of the Sydprøven granite has shown that this is not an intrusion belonging to the Gärdar alkali province, but is a genetically complex granite of   The Ilímaussaq intrusive complex in the mid-Proterozoic Gardar rift province of South Greenland is for various reasons one of the most famous alkaline plutonic complexes in the world: it is the type locality of agpaitic rocks, i.e.

of rocks with a molar ratio of (Na + K)/Al ≥ 12 (61) and with complex Na–Ti–Zr silicates (49). Abstract. The Ilímaussaq complex in South Greenland is a well-studied multiphase alkaline to peralkaline intrusion of MesoProterozoic age.

Most of the Ilímaussaq rocks are extremely enriched in alkalis, iron, halogens, high-field-strength elements (HFSE) and other rare elements, forming one of the most differentiated peralkaline rock suites ://Magmatic pulses in the emplacement of plutons Magmatic pulses in the emplacement of plutons Harry, W.

T.; Richey, J. E. Doubt is cast on the general assumption that individual plutonic units were each emplaced in one intrusive act. Lack of internal contacts does not prove this ://  1 1 Compositional variation of apatite from rift-related alkaline 2 igneous rocks of the Gardar Province, South Greenland 3 4 Revision 2 5 6 Sara Ladenburger1, Michael A.W.

Marks1,*, Brian Upton2, Peter Hill2,+, Thomas 7 Wenzel1, Gregor Markl1 8 9 1 Eberhard Karls Universität Tübingen, Mathematisch-Naturwissenschaftliche 10 Fakultät, FB Geowissenschaften, Wilhelmstra D