 | | Journal (article/letter/editorial) | | Geology of the Fana-Krossnes Area, West Coast of Norway By R. P. SHARMA,GSttingen, and B. A. STURT,Bergen...Geologisk Institntt-A, Universitetet i Bergen 5000, Norway. 62 / / ~ "~ (~H2 //~; ~~176 Kundschau~...Kundschau~ ~-~ ~0~~ Geologische !" ,,.:::: ~k/\\ 4 ~ ........ ................) I ......... .):~..~_...'? .... ,' ,{5 .... ,..... 4~6 " 6 ..... k, ....... ~ " .... ~ Cleavage 135~ + + + ....xeno(iths, amph bo tes and gneisses Sense of movement k Conjugale and kink sets-planar -w-~ --~. "~ ~] L |  | | Journal (article/letter/editorial) | | strongly deformed in the constrictional field with K values between ~3 and ~7. The constrictional deformation... biotite; Cd, cordierite; Di, diopside; Ksp, K-feldspar; Phl, phlogopite; Tr, tremolite; Wo, wollastonite...marble; Musumeci et al., 2015) and 6.14 ± 0.64 Ma (K/Ar on nappe (e.g. Barberi et al., 1967; Garfagnoli...between 1.17 and 1.38 on YZ sections (Table 1). The K value of Flinn (1965) was derived 4 | STRAIN ANALYSIS...(samples IESP3SP161, IESP3SP162 and IESP3SP164; K= shown in Figure 2a), representative of all the exposed |  | | Report (chapter) | | University of Bergen, Allegaten 41, 5007 Bergen, Norway (e-mail: haakon.fossen@geo.uib.no) Abstract: Extensional...zones, of which the largest system is located in SW Norway and related to exhumation of the subducted margin...the area between the Western Gneiss Region of SW Norway and the Fjord Region of East Greenland. Kinematic...orogenic belt. The Caledonian orogen as exposed in Norway, Greenland and the northern British Isles (Fig...zones elsewhere. Such observation were made in SW Norway, where Devonian basins were located above a metamorphic |  | | Journal (issue) | | publishing channel of all scientific meetings held in Norway with a geological content. Editors: Hans Arne Nakrem...Norges Geologiske Undersøkelse N‐7491 Trondheim, Norway E‐mail: ngf@geologi.no www.geologi.no Published...Norges Geologiske Undersøkelse N‐7491 Trondheim, Norway E‐mail: ngf@geologi.no www.geologi.no NGF Abstracts...Abstracts and Proceedings Of the Geological Society of Norway Number 1, 2017 Vinterkonferansen 2017 Oslo, January...Petroleum Guri V. Ganerød, Geological Survey of Norway Dag Helland Hansen, Aker BP Jean Sebastien L’Herureuz |  | | Report (issue) | | hornblende, muscovite, and to a lesser degree feldspar in the form of porphyroblasts which include and...to biotite schist and resulted in the growth of feldspar and muscovite in aureoles around some pegmatite...in the quartz content and plagioclase/potassium feldspar ratio of the phenocrysts, suggesting a variation...quartzose sediment, possibly as illite, potassium feldspar, or both; or (2) potassium was introduced during...sharp contact with quartzite free of muscovite and feldspar, a relationship not particularly in harmony with |  | | Report (volume) | | zone in northern Sweden CONNELLY, J. N. & AHALL, K.-I. The Mesoproterozoic cratonization of Baltica —...Mesoproterozoic anorogenic magmatism in southern Norway CONNELLY, J. N., BERGLUND, J. & Larson, S. A....flakes within the Caledonide Orogen of south-central Norway 359 Fircues, W. R., PEARCE, N. J. G., Evans,...and Ar—Ar analysis of biotite, hornblende and K-feldspar for Trans-Hudson orogen studies. This table...publication number 700. References 1995, U-Pb ANSDELL, K. M. & Norman, A. R. geochronology and tectonic development |  | | Report (issue) | | of the Norwegian Caledonides in Helgeland, North Norway. The study is divided into tvo main parts; the...zubcliviBian ot tlie metamorpnic tacieB in tne area. k^nBliBli Bummarv i8given 2t tne en6ot me paper. f ...BkogbevokBt og overgrodd, til delB dekket av reBente urer. k^ellomradene, derimot, er Btort Bett renBkrapet av...va BvovelkiB, xink blende og blvglanB, nar vZert k)ent Biden 1914. ved I^(?I^ i I^rondneim ovvbevarer...og tremolit, alle mineralene nvite til vannklare. k^nlieite ciolomitmarmorer lcan na et 8a nsiivt l^vartBinnnol6 |  | | Book | | flattened rhombohedrons (resembling those of Froland, Norway) to 12 cm across, some individuals weighing up...massive calcite. or, rarely, still attached to the feldspar/mica walls of the dike (www.davidkjoyceminerals...richterite (Menezes and Martins, 1984). EUROPE NORWAY Omdal, Froland, Aus~Agder. Thick-tabular to equant...(Moore, 1991). Old labels often give "Arendal, Norway" as the locality for these ilmenite specimens,...specimens in which euhedral crystals of andesine feldspar, augite and ilmenite rest on matrix of fine-grained |  | | Book | | correlations: Britain and Scandinavia H1GGINS, A. K. & PHILLIPS, W. E. A. East Greenland Caledonides--an...339 Contents vii WINCHESTER,J. A. & WHITTLES,K. H. The pattern of three-dimensional metamorphism...Irish Silurian rocks 423 ALDRIDGE, R. J., DORNING, K. J., HILL, P. J., RICHARDSON, J. B. • Microfossil...O L O G Y HOLLAND,C. H., KELLING,G. & WALTON,E. K. O. T. Jones and after: A multitude of models 469...LEGGETI, J. K. Oceanic sediments from the Ordovician of the Southern Uplands 495 LEGGETI',J. K., MCKERROW |  | | Book (edition) | | useful! SI prefixes commonly used in this text are k = kilo-, 10 3 ; M = mega-, 10 6 (million); G = giga-...4 7.2 6.4 Rank Commodity 23 24 25 Fluorite Feldspar Baryte 26 Titania 27 28 Asbestos Fuller's...of industrial and ore 200 1950 7 Aluminium Feldspar Lead Phosphate Sulphur Trona Cobalt Gold Mica...fluor-compounds, industrial diamonds, iodine, and feldspar and silica in the form of glass; so prices will...Commodity 1965 1975 1983 Asbestos Baryte Diatomite Feldspar Fluorspar Graphite flake Gypsum Kaolin Mica (ground) |  | | Book | | A. Bodenhausen, G.J. Borradaile, J. D. Byerlee, K. A. W. Crook, G. A. Davis, J. F. Dewey, M. A. Etheridge...normal and shear components of stress across P are K| = '^'=crcos 2 0=-jcos 2 Ap A and (1.6) If I ...designate the principal axes of the strain ellipsoid \ lt k 2 and corresponding to the maximum, intermediate,...principal In this X3 , , axes, respectively. k u k 2 , ^3 are the principal quadratic elongations...illusprincipal axes of the strain ellipsoid are parallel to k lf k 2 , trated in Figure 1.13. 1. Axially symmetric |  | | | | PUT Figure 4. PRO C E S S RES P 0 N S E B LAC K BOX OUT PUT Simple cybernetic model of inputblack...weathered granitic material containing 60 percent K-spar. This material passes through the black box labeled...types of output, which differ in proportion of feldspar from much less, to 12 GRIFFITHS much more...which the source material differs in proportion of feldspar, a fairly reasonable expectation under "real world"...contains no feldspar and is equifinal. The fact that a detrital sediment contains no feldspar does not permit |  | | Book | | The input granitic material containing 60 percent K-spar. This material passes through the black box labeled...types of output, When ditter an proportion of feldspar from much less, to GRIFFITHS | 12 much more...which the source material differs in proportion of feldspar, a fairly reasonable expectation under "real world"...contains no feldspar and is equifinal. The fact that a detrital sediment contains no feldspar does not permit...permit us to infer that there is no feldspar in the source area, another example of the phenomenon of |
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