ÅRSMELDING 2017

Fiq.l , This figure illustrates the type s of impurities th at are comm on in quartz, The left part of the figure illustratesdifferent type s of impurities, Le, solid inclusions,

Again, like us, they observed that radon levels are similar in dwellings on different carbonatite types and they suggested that high indoor radon concentrations were caused by

In the other boreholes apparent permeabilities in the region of 10" rn/s are obtained for the bore hole sections below the transmissive near-surface fractures, agreeing well

It follows, which a large body of geomorphological literature also shows, that Quaternary glaciations have eroded the landscape selectively (e.g., Sugden 1978, Nesje and

Tills deposited during a MIS 5d glaciation (c. 100–110 ka) No deposits from Weichselian glacial advances prior to LGM 2 have been recorded on Varangerhalvøya, northern and east-

Neotectonics in Norway are characterised by: 1) geological features: two documented postglacial faults in northern Norway; Neogene doming of sedimentary depocentres in the Vøring

Neotectonics in Norway are characterised by: 1) geological features: two documented postglacial faults in northern Norway; Neogene doming of sedimentary depocentres in the Vøring

The asymmetric folds (F3) which fold the mylonitic fabric in the area are well developed within the Gamlehaugen Comp- lex, and show the same geometrical features as in the