 | | Report (chapter) | | granites of the Mykle region in the southern part of the Oslo igneous province, Norway BERNARD BONIN &...granites of the Mykle region in the southern part of the Oslo igneous province, Norway. Norges geologiske...Bulletin 441, 17–24. The granites exposed around lake Mykle constitute two discrete massifs. The western...about 75 % of the area of the Oslo Rift of southern Norway (Oftedahl 1978). Granites make up about 20% of...can be observed at Eidanger, about 30 km south of Mykle (unpublished observation), represents the southernmost |  | | Journal (article/letter/editorial) | | Net-veined complexes in the Oslo Rift, southeast Norway V. M o r o g a n a a n d H. Sorensen b "Department...known as net-veined complexes has been found at Lake Mykle in the southwestern part of the late Paleozoic...southwestern part around the northern part of Lake Mykle, in contact zones between ekerite (peralkaline...the Oslo Rift, located on the western shore of Lake Mykle at Flinteodden (Fig. 1). Field relations The...complexes on the western shore of Lake Mykle and to the north of that lake occur in the contact zones between |  | | Journal (article/letter/editorial) | | University of Oslo, P.O. Box 1047 Blindern, N-0316 Oslo, Norway School of Earth & Environmental Sciences, University...evolving from sodic hedenbergite to zirconium-rich aegirine, arfvedsonite and siderite. During postmagmatic...and 6). The overall trend from hedenbergite to aegirine in groundmass and vein pyroxene (Fig. 5a) suggests...monzonite (larvikite) and syenite in the Oslo Rift, Norway (Andersen, 1984; Andersen and Sørensen, 2005; Neumann...1988). a: Variation in the diopside–hedenbergite–aegirine projection. Di = CaMgSi2O6, Hd = CaFeSi2O6, Aeg |  | Kempe, U., Möckel, R., Graupner, T., Kynicky, J., Dombon, E. (2015) The genesis of Zr–Nb–REE mineralisation at Khalzan Buregte (Western Mongolia) reconsidered. Ore Geology Reviews, 64. 602-625 doi:10.1016/j.oregeorev.2014.05.003 | Journal (article/letter/editorial) | | are situated adjacent to the north-western end of Lake Khar Us Nuur, about 45 km NE from the centre of...located within a paleoarc structure forming the Lake tectonic zone and occur near the contact with the...Mongolian Altai Range. The rocks of the paleoarc of the Lake zone represent the main host rocks to the alkaline...related regional structures tend north-south in the Lake zone and in adjacent areas of the Mongolian Altai...and Yarmolyuk, 1995). Alkaline magmatism in the Lake zone occurs within a north-south trending graben-like |
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