17 results
Distribution of rock fragments, grain size and chemical elements of tills in the Lake Mjøsa area, eastern NorwayBjørn A.
Geology and structural evolution of the Precambrian rocks of the Oslofjord - Øyeren area, Southeast Norway.Ole GraversenPage(s): 1-50 + ka
A U-Pb zircon, Archaean age for granitoid rocks in the Kunes Nappe, Laksefjord Nappe Complex, Finnmark, North NorwayDavid Roberts, L.
TrønderEnergi har, i samarbeid med Oppdal og Sunndal komrnuner, gjennomført et prosjekt med sikte på å endre deler av manøvreringsreglementet for Driva kraftverk i Sunndalen. Gjevilvatnet er hovedmagasin for kraftverket og målet med endringene i reglementet er å bedre fyllingsforholdene i magasinet ved å minske pålagt slipping av magasinvann til Driva elv i sommerhalvåret. Regulanten ønsker gjennom dette å imøtekomme klager fra grunn-og hytteeiere angående påståtte ødeleggelser, bl.a.
Middle and Late Pleistocene stratigraphy, chronology and glacial history in Finnmark, North Norway.Lars Olsen, Vagn Mejdahl, Synøve F.
QuarryScapes: ancient stone quarry landscapes in the Eastern Mediterranean. IntroductionNizar Abu-Jaber, Elizabeth G.
Age of the Younger Dryas ice-marginal substages in Mid-Norway - Tautra and Hoklingen, based on a compilation of 14C-datesLars Olsen, Fredrik Høgaas, Harald SveianPage(s): 1-13
Jordskorpen kan bevege seg så kraftig at det oppstår sprekker, forkastninger og knust berg. Slike partier kalles ofte bruddsoner. Ulike deler av bruddsoner har karakteristiske trekk.
Geological note: Petrophysical and thermal properties of pre-Devonian basement rocks on the Norwegian continental marginTrond Slagstad, Cécile Barrére, Børre Davidsen, Randi K.
Glacial landforms and Quaternary landscape development in NorwayOla Fredin, Bjørn Bergstrøm, Raymond Eilertsen, Louise Hansen, Oddvar Longva, Atle Nesje, Harald SveianPage(s): 5-26
Forkortet: The Varanger Peninsula is underlain by weakly metamorphosed sedimentary rocks of Late Proterozoic to Early Cambrian age. The rocks occur in two regions: the Tanafjorden-Varangerfjorden Region (TVR) (southwestern half of the penin- sula) and the Barents Sea Region (BSR) (northeastern half), juxtaposed along a complex NW-SE-trending fault zone, The Trollfjorden-Komagelva Fault Zone (TKFZ).
Paleogene fossils in erratic blocks from Averøy and Frei, Nordmøre, NorwayM. Smelror, À.
Upper Palaeozoic lithostratigraphy of the Southern part of the Norwegian Barents SeaGeir B. Larssen, Geir Elvebakk, Leif B. Henriksen, Stein-E. Kristensen, Inger Nilsson, Tommy J. Samuelsberg, Tore A.
Genesis of magmatic oxide deposits - a view from the Busveld complexGrant CawthornePage(s): 11-21Titanium deposits in Ukraine focused on the Proterozoic anorthosite-hosted massifs.Dmitry Gursky, Sergey
This volume of NGU Special Publication presents some of the ongoing research at the Geological Survey of Norway and shows how geology and geological knowledge influence many areas of society. The global demand for geological resources is on the rise, and knowing where to look for these resources is becoming increasingly more important. In addition, quantifying these resources is vital to ensure present-day as well as future supplies.