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Wednesday, May 13, 2020 | History

2 edition of Petrology and Geology of the Precambrian Gardar Dykes on Qaersuarssuk, South Greenland. found in the catalog.

Petrology and Geology of the Precambrian Gardar Dykes on Qaersuarssuk, South Greenland.

Geological Survey of Greenland.

Petrology and Geology of the Precambrian Gardar Dykes on Qaersuarssuk, South Greenland.

by Geological Survey of Greenland.

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  • 3 Currently reading

Published by s.n in S.l .
Written in English


Edition Notes

1

SeriesGeological Survey of Greenland Report -- 14
ContributionsWatt, W.
ID Numbers
Open LibraryOL21791203M

As one of the largest alkaline-carbonatite provinces on Earth (Fig. ), the Devonian Kola Alkaline Province (KAP) provides an ideal opportunity to evaluate the various models that have been proposed for the origin of carbonatitic atites at Kola are widespread, occur in many forms, and almost all are associated with a wide variety of silicate rocks. Roadside Geology of Wales Dinorwic slate quarries. Igneous dyke in slate: Vivian slate quarry Llanberis. Llanberis. Precambrian Padarn volcanic ash outcrops. Geological map of Pass of Rhyd-Ddu. Mynydd Mawr. Geology of File Size: 1MB.

This chapter describes tectonic evolution in the Precambrian. An analysis of the Precambrian sequences of the continents of the Southern Hemisphere is presented along with a compilation of proposed correlations according to the scheme used for the Northern Hemisphere. Bd. / Nr. 3 / Watterson, J. / PLUTONIC DEVELOPMENT OF THE Ilordleg Area, South Greenland, Part 2, Late Kinematic basic dykes, København, , pb, pages, 39 figs., 4 plates, 4 tables, - 3 -, $ 25 End of the Greenland and the North Atlantic Geology Catalog. Click any link to contine International Geology Home Page.

Major events are the formation of grabens (Keweenewan, Seal Lake, Gardar, Figs. , ) and the intrusion of basic dyke swarms. The earliest activity was apparently in the Seal Lake graben ( f 92Ma; Baragar, b) and in its approximate continuation in Greenland, the Gardar region (Berthelsen and Henriksen, ; Fig. ).Cited by: 7. The palaeomagnetism of middle Proterozoic dyke swarms of the Gardar Province and Mesozoic dykes in SW Greenland: Geophys. J. Int. Piper and Zhang () Piper, J.D.A., Zhang, J. Palaeomagnetism, rock magnetism and magnetic fabric in Precambrian metamorphic terranes of the Huabei Shield, China: J. Asian Earth Sci.


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Petrology and Geology of the Precambrian Gardar Dykes on Qaersuarssuk, South Greenland by Geological Survey of Greenland. Download PDF EPUB FB2

Petrographic and radiographic analyses were conducted on oriented samples of Late Precambrian-Cambrian quartzose sandstones collected from five cratonal and five miogeoclinal stratigraphic sections in the eastern Mojave Desert, southeastern California.

Twelve petrographic variables were measured in each of by: 6. This wide-ranging discussion of Precambrian rocks includes contributions from a diverse array of authors actively engaged in investigations of various aspects of U.S.

Precambrian geology. Summary discussions by the editors of the five major chapters place these contributions in a logical regional framework. Halama R, Waight T, Markl G () Geochemical and isotopic zoning patterns of plagioclase megacrysts in gabbroic dykes from the Gardar Province, South Greenland: implications for crystallisation processes in anorthositic magmas.

Contrib Mineral Petrol (1)– CrossRef Google ScholarAuthor: V. Sesha Sai, S. Mahapatro, Santanu Bhattacharjee, Tarun C. Khanna, M.

Korakoppa. Mafic dykes of Almora region intrude the Precambrian crystalline rocks of Kumaun Lesser Himalaya. Mafic dykes exhibit fine grained margin and medium to coarse grained core, melanocratic, low to. The intrusions and associated dyke swarms belonging to the Mesoproterozoic Gardar Province in South Greenland were emplaced during two main magmatic periods at and Ma (Upton ).

The geology and petrology of the Precambrian rocks to the north-east of the Fjord Qagssit, Frederikshåb district, south-west Greenland.

Meddelelser om Grønland ; 98 pp., 23 fig., 7 photoplts., 4 fold. plts. maps in pocket. 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: South Greenland presents a globally unique opportunity to study the remnants of ancient rift zone igneous complexes and associated volcanic rocks.

These rocks are related to the Gardar Province, a rift zone active during the Mesoproterozoic as Palaeopangea broke apart. Rifting ceased before transition into oceanic spreading and as a result the igneous products were.

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. The m thick Basistoppen sill is an Eocene, tholeiitic, layered intrusion emplaced in the upper part of the Skaergaard complex shortly after solidification of the Skaergaard magma.

Despite its small size, the Basistoppen sill has one of the most extensive differentiation sequences by: The Mesoproterozoic Gardar Province in South Greenland developed in a continental rift-related environment.

Several alkaline intrusions and associated dyke swarms were emplaced in Archaean and Ketilidian basement rocks during two main magmatic periods at – Ma and – by: Abstract.

Mafic dykes are a characteristic geological feature of the Ruker Complex in the southern Prince Charles Mountains.

We present new geological, geochemical, and Sm–Nd isotopic data for these rocks, which place constraints on their genesis, mantle sources, and relative timing, as well as providing a substantial basis for a comparison between these Cited by: 7.

Zr/Nb vs. Ce/Y diagram for Gardar basic lavas, doleritic dykes, gabbroic chilled margins, ultramafic lamprophyres and carbonatites (based on. A pattern of fractures and basic dykes occurring in an area of about km 2 of pre-Ketilidian gneisses (~ 2, m.y.) near Frederikshåb in southwest Greenland has been analysed in terms of modern views on fracture formation.

Most of the fractures are late pre-Ketilidian and they are intruded by four principal generations of by: A 'read' is counted each time someone views a publication summary (such as the title, abstract, and list of authors), clicks on a figure, or views or downloads the full-text.

Introduction. The Gardar Alkaline Igneous Province comprises a Mesoproterozoic (– Ma) suite of alkalic intrusions in southern Greenland (Upton and Emeleus,Upton et al., ).Although best known for its syenite and nepheline syenite plutons including the celebrated Ilímaussaq Complex, the province also includes some enigmatic ultramafic lamprophyres of Cited by: "Precambrian Ore Deposits of the East European and Siberian Cratons" is a sequel to "Precambrian Geology of the USSR" published in (English edition), in which the main emphasis was on the stratigraphy, magmatism and metamorphism of Precambrian assemblages in both ancient cratons (East European and Siberian) as well as in Phanerozoic fold belts and.

Progress in Precambrian geology has been exceptionally great, indeed quite striking for geologists of the older generation; only some years ago the Precambrian appeared as an uncertain and even mystic prelude to geologic by: 1.

Introduction. Wegmann () adopted the term ‘Gardar Formation’ from the old Norse bishopric of Gardar in south Greenland, as the name for the distinctive association of essentially unmetamorphosed and undeformed alkaline intrusive rocks and successions of clastic sediments and subaerial lavas which are beautifully exposed in the area.

Earlier reviews of the province Cited by: Petrology and Geology of the Precambrian Gardar Dykes on Qaersuarssuk, South Greenland.

50p light blue card cover, author note to cover, photographic illustrations, excellent condition £. Ion microprobe U-Th-Pb analyses of residual cores and metamorphic mantles of zircons from three high grade paragneisses from the Seve Nappe Complex, north-western Sweden, show that: 1) The sediments comprising the protolith of the Seve Nappes gneisses over a distance of km were probably derived from similarly-aged source terranes.

2) Those Cited by: 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 .This is a preliminary account of the geology of the Precambrian rocks in the area between 70°45' and 72°30' N on the west coast of Green­ land.

The mapping was carried out in the field seasons of and '63 as part of the systematic investigation of West Greenland being undertaken by the Geological Survey of Greenland (Grønlands Geolo­.