The Norwegian Innovation-Collaboration Survey

In v iew of th e high conten t of mafic minerals in maj or part s of th e Sogn anort hosites (Fig. 6), only rest rict ed areas are of indust rial int erest.. In th e Gudvanq en-Mj

Investigat ions of th e Moyale graphite have com prised map ping the gr aph - ite bod y by geo logical and geoph ysical meth od s, analysis of th e graph it e carbo n conten t,

On th e background of th e small num ber of deposits visited during th e 1998 fieldwor k and basic know ledge of others , it may be conclu ded that the bedroc k geology of Eritrea

The high est average linear sedi me ntati on rate (4.7 mm/ year) was found for a core (NC-84) from st at ion 67, on the southe rn lowerm ost slope of th e Norwegian Trough ; a

The igneou s rocks of the Kvamsoy area in th e sout hern part s of th e Western Gneiss Complex (WGC) of Norway comprise a wide variety of granit ic, syenitic, granodiorit ic

There is a general thinning of th e Se ve Nappe Complex nort hwards and it wedges out in th e northernm o st part of t he study area.The overlying V addas Nappe of the Koli

In the present paper, we report the discovery of a small body of subvol- canic trachyte or microsyenite on the east coast of lake Mykl e in th e southwestern part of the Oslo Rift, in

The olivin e gabb ro is enti rely enclosed w it hin a youn ger int rusion, here termed th e Layered Se ries w hich con- stitutes th e great er part of the GI C.On the basis of