1 edition of Ilímaussaq intrusion, South Greenland found in the catalog.
Ilímaussaq intrusion, South Greenland
|Other titles||Ilímaussaq intrusion.|
|Statement||edited by John C. Bailey, Lotte Melchior Larsen and Henning Sørensen.|
|Series||Contribution to the mineralogy of Ilímaussaq -- no. 63, Contributions to geology / Geological Museum of the University of Copenhagen -- no. 387, Rapport / Grønlands geologiske undersøgelse -- nr. 103, Contributions to geology (Københavns universitet. Geologisk museum) -- no. 387., Rapport (Grønlands geologiske undersøgelse) -- nr. 103.|
|Contributions||Bailey, John C. 1944-, Larsen, Lotte Melchior., Sørensen, Henning.|
|LC Classifications||QE70 .D43 nr. 103, QE70 .D43 nr. 103|
|The Physical Object|
|Pagination||130 p. :|
|Number of Pages||130|
The early augite syenite unit in the 1Ga-old Ilímaussaq intrusive complex, South Greenland, consists of a magmatic assemblage of ternary alkali feldspar + fayalitic olivine + augite. Geological Guide - South Greenland. The Narsarsuaq - Narsaq - Qaqortoq region. This book is a handy guide book to the fascinating geology of South Greenland which houses some world-famous mineral localities. It focuses on the description of the main geological features of the region and of localities and is planned as a handy guide book to be used in the field.
Semenovite, (RE, Ca, Mn, Na) 12 (Be, Si(F, OH,))) 8 (Si 3 O 10) 4 H 2 O occurs in cavities in one epi-eudidymite bearing albitite on the Taseq Slope, Ilímaussaq, Greenland. The size of the major part of the apparently tetragonal bipyramidal crytals ranges from to mm. Colour: brown, reddish brown or grey. The Ilimaussaq intrusion belongs to the late Precambrian Gardar province, south Greenland (Upton, ; Emeleus and Upton, ). In the province a series of alkaline igneous com¬ plexes occurs which evolved either towards Si-rich rocks such as comendites and granites, or towards Si-poor rocks such as phonolites and.
The Gardar province of South Greenland hosts a number of peralkaline igneous centres associated with rifting between ca. and Ma. Due to its remarkable agpaitic ([Na+K]/Al > ) mineralogy and economic potential by enrichment in REE and U, the Ilimaussaq intrusive complex has been the subject of intense study and is dated at Ma, representing late . fluids in the peralkaline Ilímaussaq intrusion, South Greenland: Lithos, , – Karup-Møller, S., J. Rose-Hansen, and H. Sørensen, , Eudialyte decomposition minerals with new hitherto undescribed phases from the Ilímaussaq complex, South Greenland: Bulletin of the Geological Society of Denmark, 58,
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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, Ilímaussaq intrusion one of the most differentiated peralkaline rock suites by: The Ilímaussaq complex in South Greenland is a well-studied multiphase alkaline to Ilímaussaq intrusion intrusion of MesoProterozoic age.
Most of the Ilímaussaq rocks are extremely enriched in alkalis. Beryllium mineralization in the Ilimaussaq intrusion, South Greenland: 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 other formats and editions Enter your mobile number or email address below and we'll send you.
The Ga Ilímaussaq intrusion (Krumrei et al., ; Fig. 1) is part of the Mid-Proterozoic Gardar rift province in South Greenland (e.g., Emeleus and Cited by: 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. The Ilímaussaq intrusion belongs to the – Ga Gardar province (Upton et al., ).The formation of the Ga old intrusion (Fig.
1a–c) is described as a succession of three magma batches from one single mantle source (Larsen and Sørensen,Marks et al., ), which intruded successively to 3–4 km depth (Konnerup-Madsen and Rose-Hansen.
TY - BOOK. T1 - Preliminary Mining Assessment of the Uranium Resource at Kvanefjeld, the Ilimaussaq Intrusion, South Greenland. AU - Kalvig, P. PY - Y1 - M3 - Book.
BT - Preliminary Mining Assessment of the Uranium Resource at Kvanefjeld, the Ilimaussaq Intrusion, South Greenland. PB - Risø National Laboratory.
CY - Roskilde. ER. Reference: pavel M. Kartashov data/ Petersen, O. V.; Rønsbo, J.G. & Leonardsen, E.S. (): Nacareniobsite-(Ce), a new mineral species from the Ilímaussaq alkaline complex, South Greenland, and its relation to mosandrite and the rinkite series. Neues Jahrbuch für Mineralogie, Monatshefte 2, ; Henning Sørensen and Lotte Melchior Larsen () The hyper.
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 mechanism.
The Ilímaussaq intrusion consists of an augite syenite shell and a central cumulitic series of layered peralkaline (agpaitic) nepheline syenites with both roof and bottom cumulates.
Microprobe analyses of the strongly zoned mafics show that the pyroxenes range from ferro-salite through hedenbergite to aegirine, the amphiboles from hastingsite. 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 ; with chemical analyses by Ib Sørensen.
Ilimaussaq intrusive complex The Ilímaussaq complex (Fig.1) is one of several alkaline complexes formed during Mesoproterozoic rifting in the southwestern part of Greenland, which collectively is called the Gardar province.
With an age of Ga, Ilímaussaq is the youngest major intrusion of the Gardar province. of the Ilímaussaq alkaline complex, South Greenland ‘The Ilímaussaq intrusion, South Green-land. A progress report on geology, mineralogy, geo-chemistry and economic geology’, published as Contribution to the mineralogy of Ilímaussaq no.
63 in Rapport Grønlands Geologiske Undersøgelse ed. 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.
90 Piper: Palaeomagnetism of the Ilimaussaq intrusion Fig. Distribution of palaeomagnetic sampling sites in the Ilimaussaq intrusion, South Greenland (°E, 61 °N).
the kakortokites but in a different part of the intrusion; Ferguson () quotes a thickness of m for this unit. Lujavrites (arfvedsonite and aegirine-bearing nepheline.
Bohse, H, Brooks, CK & Kunzendorf, HField observations on the kakortokites of the Ilimaussaq intrusion, South Greenland, including mapping and analyses by portable X-ray fluorescence equipment for zirconium and niobium.
Grønlands Geologiske Undersøgelse. (): Tuperssuatsiaite, a new mineral species from the Ilímaussaq intrusion in South Greenland, Neues Jahrbuch für Mineralogie, Monatshefte. 2 North shore, Tunulliarfik Fjord, Ilímaussaq complex, Narsaq, Kujalleq, Greenland. Ilimaussaq alkaline intrusion, South Greenland.
Bulletin of the Geological Society of Den mark Denmark, vol. 42, pp Copenhagen b Cryptorhythmic layering (Wilson ) has been established in a m drill core through a layered aegirine-eudialyte nepheline syenite, aegirine lujavrite I, of the Ilimaussaq alkaline intrusion.
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.
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. Sorensenite: A new sodium-beryllium-tin-silicate from the Ilimaussaq Intrusion, South Greenland (Meddelelser om Grønland) [Semenov, E. I] on *FREE* shipping on qualifying offers.
Sorensenite: A new sodium-beryllium-tin-silicate from the Ilimaussaq Intrusion, South Greenland (Meddelelser om Grønland)Author: E. I Semenov.A new mineral. skinnerite (Cu 3 SbS 3 with minor amounts of silver), is identical with synthetic Cu 3 SbS 3 (the B'phase of Skinner, Luce, and Makovicky, ).
A reversible phase transfoimation takes place in both materials at about l22° high tbmperature modification (B) is orthorhombic (a = l Å,b = lO Å,c = Å, space group Pnma, Z = 4); the low .Get this from a library!
Beryllium mineralization in the Ilimaussaq intrusion, South Greenland, with description of a field beryllometer and chemical methods.