2 edition of Ilimaussaq Intrusion, South Greenland found in the catalog.
Ilimaussaq Intrusion, South Greenland
Geological Survey of Greenland.
|Series||Geological Survey of Greenland Report -- 103|
|Contributions||Bailey, J., Larsen, L., Sorensen, H.|
Geography. The Ikersuaq fjord is oriented in a roughly NE/SW direction and to the southwest its mouth opens into the Julianehab Bay, Labrador Sea, North Atlantic is a vast ice field on the northwestern side of the fjord, where there are three branches, Qaleragdlit Imâ, Kangerlua and Kangerluarsuk.. The Northern Sermilik (Nordre Sermilik) fjord is the inner section of Basin countries: Greenland. Petersen, O.V. (): List of all minerals identified in the Ilímaussaq alkaline complex, South Greenland. Geology of Greenland Survey Bulletin. , Kangerluarsuk Fjord.
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One of the 10 alkaline intrusions of the Gardar Complex. Apatite containing > wt % REO has been identified. U-Be-Zr-Nb mineralization. Jackson and Christiansen classify as carbonatite. Part II: Reviews of Major Layered Intrusions - The Panzhihua Intrusion, Southwestern China.-The Sept Iles Intrusive Suite, Quebec - The Bushveld Complex, South Africa - The Kiglapait Layered Intrusion, Labrador - The Ilimaussaq Intrusion, Greenland - Ophiolitic Magma Chambers; a Perspective from the Canadian Appalachians. Customer Reviews.
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The Ilimaussaq intrusive complex is a large alkalic layered intrusion located on the southwest coast of is Mesoproterozoic in age, about Ga. It is the type locality of agpaitic nepheline syenite and hosts a variety of unusual rock types.
The complex is noted for a wide variety of rare minerals and is the type locality for thirty minerals, including: aenigmatite. Beryllium mineralization in the Ilimaussaq intrusion, South South Greenland book With description of a field beryllometer and chemical methods, (Contribution to the mineralogy of Ilimaussaq) Unknown Binding – January 1, See all formats and editions Hide Format: Unknown Binding, 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. On beryllite and bertrandite from the Ilímaussaq alkaline intrusion, South Greenland: Responsibility: by Haldis Bollingberg and Ole V.
Petersen. On beryllite and bertrandite from the Ilímaussaq alkaline intrusion, South Greenland / by Steen Andersen ; South Greenland book. Cuprostibite and associated minerals from the Ilímaussaq intrusion, South Greenland. [S Karup-Møller;] Home. WorldCat Home About WorldCat Help. South Greenland book.
Search for Library Items Search for Lists Search for # Greenland--Ilimaussaq Mountain.\/span>\n \u00A0\u00A0\u00A0\n schema. Berylium mineralization in the Ilimaussaq intrusion, South Greenland, with description of a field beryllometer and chemical methods J.
Engell, J. Hansen, M. Jensen, Helmar Kunzendorf, Leif Løvborg Research output: Book/Report › ReportAuthor: J. Engell, J. Hansen, M. Jensen, Helmar Kunzendorf, Leif Løvborg. 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 by: Abstract. The Ilimaussaq alkaline intrusion in South Greenland provides examples of various types of igneous layering.
Inch-scale layering occurs in the least differentiated rocks augite syenite and pulaskite and is probably caused by a nucleation-diffusion by: H.
SørensenBrief introduction to the geology of the Ilimaussaq alkaline complex, South Greenland, and its exploration history H. Sørensen (Ed.), The Ilimaussaq Alkaline Complex, South Greenland; Status and Mineralogical Research with New Results, Geology of Greenland Survey Bulletin, (), pp.
Cited by: 3. Reference: Karup-Moeller, S. (): Gmelinite and Herschelite from the Ilimaussaq Intrusion in South Greenland, Mineralogical Magazine, Vol.
40, Buy On the mineralogy and paragensis of tugtupite Na Al Be Si O (Cl, S), from the Ilimaussaq alkaline intrusion, South Greenland (Contribution to the mineralogy of Ilimaussaq) on FREE SHIPPING on qualified orders.
the Ilimaussaq alkaline intrusion, South Greenland. Bulletin of the Geological Society of Denmark, vol. 40, pp. Copenhagen Li was analysed by instrumental neutron activation analysis and Cerenkov counting in mineral samples (30 species) from the Ilimaussaq alkaline intrusion, South Greenland.
Marks and G. Markl Introduction The Ilímaussaq igneous complex in South Greenland is a Mesoproterozoic com-posite intrusion that mainly consists of syenitic and nepheline syenitic rocks.
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 kakortokite series 15 4. Chemistry of the layered kakortokite series 19 5.
1. Layering in the Ilimaussaq Alkaline Intrusion, South Greenland.- 2. Layering, Compaction and Post-Magmatic Processes in the Klokken Intrusion.- 3. Gabbroic, Syenogabbroic and Syenitic Cumulates of the Tugtutôq Younger Giant Dyke Complex, South Greenland.- 4. A Large Soft-Sediment Fold in the Lilloise Intrusion, East Greenland.- : Gamma-ray spectrometry in the field was used in connection with an intensive study of the abundance and distribution of U and Th in peralkaline rocks of Cited by: In time, there were about 5, settlers in Greenland.
The official records indicate that two sizable Norse settlements had been founded in fjords on the southwestern coast of the island. Other smaller ones were located on the same coast as far north as present day Nuuk. Layering in the Ilimaussaq Alkaline Intrusion, South Greenland.- 2.
Layering, Compaction and Post-Magmatic Processes in the Klokken Intrusion.- 3. Gabbroic, Syenogabbroic and Syenitic Cumulates of the Tugtutoq Younger Giant Dyke Complex, South Greenland.- 4. A Large Soft-Sediment Fold in the Lilloise Intrusion, East Greenland.- 5. Ilimaussaq Alkaline Complex, South Greenland: An Overview of Years of Research and an Outlook by Henning Sorensen Unknown, 70 Pages, Published ISBN / ISBN / The Zr-Y-U stratigraphy of the kakor- tokite-lujavrite sequence, southern Ilimaussaq intrusion.
Rap Author: Henning Sorensen. Distribution: In the Il³maussaq intrusion, at Tuperssuatsiait Bay, Kangerdluarssuk Fjord, and the north shore of Tunugdliar¯k Fjord, southern Greenland.
From the Aris quarry, about 25 km south of Windhoek, Namibia. In Canada, from near Saint-Amable, Quebec. Name: For Tuperssuatsiait Bay, Greenland.
10, 3, / Internal structures and geological setting of the three agpaitic intrusions: Khibina and Lovozero of the Kola Peninsula and Ilímaussaq, South Greenland; The differentiation of agpaitic magmas: the Ilímaussaq Intrusion, South Greenland; Experimental studies bearing on the origin of the alkalic rock - Carbonatite complex and.Elemental mass balance during alteration of eudialyte ore The strongly layered kakortokites of the Ilímaussaq intrusion.
The giant rare-earth element (REE) and zirconium, a.o. deposits in the Ilímaussaq intrusion in South-West Greenland include the 'Kringlerne' eudialyte deposit.Zone is used for a p~rt of an intrusion characterized by a special mineral assemblage (Hessp. 49). The layering of the peralkaline agpaitic nepheline-syenites of the Illmaus- saq intrusion, South Greenland, and the Lovozero intrusion, the Kola Cited by: