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2 edition of Geology and structure of the area west of Fyresvatn, Telemark, Southern Norway. found in the catalog.

Geology and structure of the area west of Fyresvatn, Telemark, Southern Norway.

D. V. Venugopal

Geology and structure of the area west of Fyresvatn, Telemark, Southern Norway.

The precambrian rocks of the Telemark area in South Central Norway no. X

by D. V. Venugopal

  • 98 Want to read
  • 24 Currently reading

Published by Universitetsforlaget in Oslo .
Written in English

    Places:
  • Norway,
  • Telemark fylke.
    • Subjects:
    • Geology -- Norway -- Telemark fylke.

    • Edition Notes

      Bibliography: p. 56-57.

      Statementby D.V. Venugopal.
      SeriesNorges geologiske undersøkelse ;, Nr. 268, Norges geologiske undersøkelse (Series) ;, nr. 268.
      Classifications
      LC ClassificationsQE281 .A2 nr. 268
      The Physical Object
      Pagination57 p.
      Number of Pages57
      ID Numbers
      Open LibraryOL5339178M
      LC Control Number72192778

      The farm is situated at an altitude of meters above sea level at the west and sunny side of the highest mountain in the southern part of Norway, the magnificent Gaustatoppen with its underlying geology and the overall prospectivity of a project area. Unlike many other exploration techniques, geological mapping has a fast turnaround time and provides focused drill targets in a matter of weeks. By avoiding poorly defined exploration targets, you can maximise your return and save both money and time.

      The Finnish area just east of Bothnian Bay stand out as the largest plain in the Nordic countries. The Scandinavian Mountains dominate the landscape of Norway. The southern part of the Scandinavian Mountains is broader than the northern one and contain higher peaks. The southern part contains also a series of plateaux and gently undulating. Vol. X - ANDERSON, OLAF. The genesis of some types of feldspar from granite pegmatites. Norsk Geol. Tidsskr. X; pp. , 9 fig. 9 photoplts. h.t.

      Telemark Norway (1) United Kingdom Southern Norway (1) Paleozoic subduction-related magmatism in the Duobagou area, Dunhuang block: Constrained by zircon U-Pb geochronology and Lu-Hf isotopes and whole-rock geochemistry of metaigneous rocks. Book Chapter (6) Article Type. Facet list. Research Article Southern Norway (1) Telemark Norway Bamble Norway (2) Western Gneiss region (1) United Kingdom.


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Geology and structure of the area west of Fyresvatn, Telemark, Southern Norway by D. V. Venugopal Download PDF EPUB FB2

The map area described in this account is situated west of Fyresvatn in Telemark, Southern Norway, between latitudes 58°50' and 59°15'N and longitudes 7°55' and B°2o' E.

It is bounded on the east side by the valley of Setesdal. Tovdal marks the southern boundary and Songedalsdalen the northern extremity of the area. Get this from a library.

Geology and structure of the area west of Fyresvatn, Telemark, Southern Norway. The precambrian rocks of the Telemark area in South Central Norway no. [D V Venugopal]. Fig. Structure map of the Fyresvatn area. Shaded formation is the Nape Amphi­ bolite.

The Fyresvatn Granite (+ symbol) is shown in the southern part of the area. Structure sections A-A', B-B' and C-C' are given in Fig. A geologic map at the same scale (Stoutfig. 2) is available. Tidsskr., 55, ANON. Sweden's case study for the United Nations conference on the human environment.

Air pollution across national boundaries. The impact on the environment of sulfur in air and precipitation. Stockholm, Kungl. Boktryckeriet. VENUGOPAL, D. Geology and structure of the area west of Fyresvatn Telemark Cited by: Magma mixing, structure, and re-evaluation of the emplacement mechanism of Vrådal pluton, central Telemark, southern Norway Article (PDF Available) in Norsk Geologisk Tidsskrift 78(4) Venugopal, D.V.

() ‘Geology and structure of the area west of Fyres- vatn, Telemark, southern Norway’. Norges geol. Unders,53– Google Scholar. Holocene shorelevel displacement in Telemark, southern Norway: Bjørg Stabell A Rb/Sr whole-rock isochron date from the lowermost gneiss complex of the Gaular area, west Norway and its regional implications: Finn J.

Skjerlie The Precambrian rocks of the Telemark area in south central Norway XIV: Structure and metamorphism of Precambrian. Western Norway (Norwegian: Vestlandet, Vest-Norge, Vest-Noreg) is the region along the Atlantic coast of southern consists of the counties Rogaland, Vestland and Møre og region has a population of approximately million people.

The largest city is Bergen and the second-largest is ically the regions of Agder, Vest-Telemark, Hallingdal, Valdres and. The volcanic-sedimentary Telemark supracrustal rocks form a major, ca. km-thick, basin infill in the Telemark Block (Dons, a, Dons, b, Sigmond et al.,Laajoki et al.,Bingen et al.,Bingen et al., ).They have been metamorphosed under low-grade greenschist-amphibolite facies (Atkin and Brewer,Brewer and Atkin, ).The Telemark supracrustal.

Laser ablation ICPMS U–Pb and Lu–Hf isotope data on granitic-granodioritic gneisses of the Precambrian Vråvatn complex in central Telemark, southern Norway, indicate that the magmatic. Falkum, T. The structural geology of the Precambrian Homme granite and the enveloping banded gneisses in the Flekkefjord area, Vest-Agder, Southern Norway.

Norway (Norwegian: Norge or Noreg) is the westernmost, northernmost — and surprisingly also the easternmost — of the three Scandinavian countries. Norway is known for the complex and deep fjords along its west coast, as well as the midnight sun and Northern Lights. The overall impression of Norway is a country with ample space and unusually rugged landscape.

Norway, country of northern Europe that occupies the western half of the Scandinavian half of the inhabitants of the country live in the far south, in the region around Oslo, the two-thirds of Norway is mountainous, and off its much-indented coastline lie, carved by deep glacial fjords, s islands.

Norway is a country located in Northern Europe on the northern and western parts of the Scandinavian majority of the country borders water, including the Skagerrak inlet to the south, the North Sea to the southwest, the North Atlantic Ocean (Norwegian Sea) to the west, and the Barents Sea to the north.

It has a land border with Sweden to the east and a shorter border with Finland. Silurian of the Ringerike area, south Norway. Stout, James H.: Structure and metamorphism of Precambrian rocks east of Fyresvatn.

The Precambrian rocks of the Telemark area in south central Norway XIV Salter, D. & Appleyard, E. C.: An occurrence of vein palygorskite from the nepheline syenite at Lillebugt, Stjernøy, northern. Bryggen in Bergen. The beautiful wooden buildings that overlook the bay Vågen remains one of Bergen’s central meeting points to this day.

The area dates back to when the city was founded by King Olaf III, known as Olav Kyrre. AroundBergen became an economical and administrative hub in Norway, with Bryggen as an increasing centre of commerce. Clicking on a fault brings up a popup with information describing the fault. At the bottom of the popup is the option to view a reference table which lists citations associated with the fault.

Norway has a total area ofsquare kilometres (, sq mi) and a population of 5, (as of August ). The country shares a long eastern border with Sweden (1, km or 1, mi long). Norway is bordered by Finland and Russia to the north-east, and the Skagerrak strait to the south, with Denmark on the other side.

The discipline of structural geology studies the architecture of the solid Earth and other planets. Rock deformation patterns are exciting features beacause of their aesthetic beauty and their economic interest to man.

Knowledge of the subsurface structure is vital for the success of a variety of engineering and mineral exploration pograms. Map of eastern Texas, southern Arkansas and western Louisiana showing major structural features, updip limit of Louann Salt, and oil and gas resource appraisal area 6 4.

Generalized cross section of northern Gulf of Mexico margin 8 5. Map of east Texas salt-diapir and salt-pillow provinces. One zone named the Crest fault by J. D. Forrester (, p. ), extends west to east for many miles along the west dome of the anticline just north of the crest (fig.

61). Recent mapping by Crittenden, Wallace, and Sheridan (, plate 1) showed that the Crest fault is a complex zone of many interrelated fractures with various trends and.Western Norway (Norwegian: Vestlandet, Vest-Norge, Vest-Noreg) is the region along the Atlantic coast of southern consists of the counties Rogaland, Hordaland, Sogn og Fjordane, and Møre og region has a population of approximately million people.

The largest city is Bergen and the second-largest is ically the regions of Agder, Vest-Telemark.The Ray Mears' Real Heroes of Telemark TV series demonstrated the bravery of a small group of Norwegian saboteurs during WWII who put their lives at risk to stop the Germans gaining access to a substance called Deuterium Oxide or 'heavy water', a secret ingredient crucial in the Nazis attempt to make an Atomic Bomb.