Zobrazeno 1 - 10
of 32
pro vyhledávání: '"Tore Prestvik"'
Publikováno v:
SK103-SK120
Interpretation
Interpretation
Continental breakup between NW Europe and Greenland (~56 Ma) ago was associated with widespread magmatism. Silica undersaturated alkaline porphyritic igneous rocks of a similar age have previously been dredged near the mid-Norwegian coast. These igne
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c32e5b58752940715d748596fe08a3cd
http://hdl.handle.net/10852/61061
http://hdl.handle.net/10852/61061
Publikováno v:
Geological Society, London, Special Publications. 390:583-602
The Helgeland Nappe Complex (HNC), part of the Uppermost Allochthon of the northcentral Norwegian Caledonides, originated near the Laurentian margin and was transferred to Baltica during the closure of Iapetus in Late Silurian–Early Devonian time.
Autor:
Tore Prestvik, David Chew, Valentin R. Troll, M. A. Smethurst, Morgan Ganerød, Fiona C. Meade, Fernando Corfu
Publikováno v:
Chemical Geology. 286:222-228
The British–Irish Palaeogene Igneous Province (BIPIP) is part of the larger North Atlantic Igneous Province and includes the lava fields of Antrim, Mull, and Skye. The Tardree Rhyolite Complex (TRC) in Northern Ireland forms an important stratigrap
Autor:
Joel A. Baker, Kresten Breddam, David W. Peate, Mark D. Kurz, Abigail K. Barker, Nathalie Grassineau, Tore Prestvik, Anna Cecilie Skovgaard
Publikováno v:
Journal of Petrology. 51:1447-1475
We present compositional data on a suite of 18 primitive neovolcanic alkali basalts from three flank-zone regions in Iceland (Vestmannaeyjar in the south, Snaefell in the east, and Snaefellsnes in the west) that are peripheral to the main rift zones
Autor:
Calvin G. Barnes, Lindy McCulloch, Aaron S. Yoshinobu, Yujia Li, Carol D. Frost, Tore Prestvik
Publikováno v:
Geosphere. 5:286-301
The Hortavaer intrusive complex, Norway, is a layered igneous complex that was assembled by multiple injections of magmas that ranged from gabbroic through granitic in composition. Layering is defined by intrusive sheets that range from 10 cm to 2 m
Autor:
Tore Prestvik, Håkon Austrheim
Publikováno v:
Lithos. 104:177-198
Ophiolite complexes in mountain chains may give supplementary information on the hydration of the oceanic lithosphere to that obtained from dredged and drilled samples from the ocean floor. The ultramafic (mantle) and the layered ultramafic to anorth
Publikováno v:
Earth and Planetary Science Letters
Earth and Planetary Science Letters, Elsevier, 2008, 272, pp.464-475. ⟨10.1016/J.EPSL.2008.05.016⟩
Earth and Planetary Science Letters, Elsevier, 2008, 272, pp.464-475. ⟨10.1016/J.EPSL.2008.05.016⟩
International audience; The paleomagnetic data sets from the British Tertiary Igneous Province (BTIP) have recently been criticized as being unreliable and discordant with data from elsewhere in the North Atlantic Igneous Province (NAIP) [Riisager et
Publikováno v:
Lithos. 80:179-199
The intrusive complex at Hortav&r represents a magma transfer zone in which multiple pulses of gabbroic and dioritic magmas evolved along Fe- and alkali-enrichment trends. Extreme alkali enrichment resulted in nepheline-normative and sparse nepheline
Publikováno v:
Lithos. 75:389-412
The Sausfjellet pluton is made up of two intrusive units emplaced into high-grade metamorphic rocks of the Helgeland Nappe Complex of the Uppermost Allochthon in the Norwegian Caledonides. The eastern part of the pluton intruded marble and less volum
Autor:
Haraldur R. Karlsson, Tore Prestvik, Øystein Nordgulen, Calvin G. Barnes, Aaron S. Yoshinobu, Bjørn Sundvoll
Publikováno v:
Journal of Petrology. 43:2171-2190
distinct, with Nd and O in the migmatites from −7·6 to −9·6 The dioritic Velfjord plutons (>448 Ma) were emplaced into and from +10·9‰ to +13·5‰, and in the contact granites regional migmatitic metapelitic and metacarbonate rocks at midfr