Sökning: "Sydvästra Värmland"

Hittade 3 avhandlingar innehållade orden Sydvästra Värmland.

  1. 1. Myrvegetation i sydvästra Värmland

    Författare :Sven Fransson; Uppsala universitet; []
    Nyckelord :NATURVETENSKAP; NATURAL SCIENCES; Wetlands; Swamps; Våtmarker; Växtekologi; myrar; Växtsamhällen;

    Sammanfattning : .... LÄS MER

  3. 2. Förflutna rum : landskapets neolitisering i sydvästra Värmland : Rooms of the past. The neolithization of the landscape in southwestern Värmland, Sweden

    Författare :Curry Heimann; Göteborgs universitet; []
    Nyckelord :HUMANIORA; HUMANITIES; Neolithization; landscape archaeology; Värmland; Late Neolithic; stone cists; gallery graves; architectural theory; Rock Art; pollen analysis; Western Sweden;

    Sammanfattning : The main objective of this thesis is to study the effect of the Stone Age neolithization process on the human landscape. The landscape should here not be reduced to an arena for human actions provided by nature, but instead be viewed as something continuously being created by man, in a mental as well as in a physical sense. LÄS MER

  4. 3. Sveconorwegian orogenesis in the southwestern Baltic Shield - Zircon geochronology and tectonothermal setting of orthogneisses in SW Sweden

    Författare :Jenny Andersson; Berggrundsgeologi; []
    Nyckelord :NATURVETENSKAP; NATURAL SCIENCES; Petrology; Geologi; fysisk geografi; physical geography; Geology; structural markers; augen gneiss; orthogneiss; migmatite; ion microprobe; Pb-Pb evaporation; U-Pb; geochronology; zircon; Sweden; Mylonite Zone; Western Segment; Sveconorwegian orogen; Eastern Segment; mineralogy; geochemistry; Petrologi; mineralogi; geokemi;

    Sammanfattning : The Mylonite zone (MZ) is a prominent late-Sveconorwegian lithological terrane boundary in the SW Baltic Shield along which large-scale crustal block movements took place during the Sveconorwegian orogeny. The southern section of the MZ also defines a conspicuous metamorphic break separating upper amphibolite and high-pressure granulite facies rocks in the parautochthonous Eastern Segment (ES), from middle amphibolite facies rocks in the overlying Western Segment (WS). LÄS MER