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  • Oligocene tuffs at Domžale, the Ljubljana basin, Slovenia = Oligocenski tufi pri Domžalah
    Kralj, Polona ; Grad, Karel
    Oligocene volcanics have not been found yet in the Ljubljana basin. At Domžale, fine-grained tuffs predominate, although coarse-grained and lapilli tuffs also occur. The main constituents are ... volcanic glass shards. The tuffs are rhyolitic in composition. Alteration is reflected in the development of clay minerals - calcic montmorillonite and illite.
    Vir: Geologija. - ISSN 0016-7789 (vol. 43, 2, 2000, str. 219-221)
    Vrsta gradiva - članek, sestavni del
    Leto - 2000
    Jezik - angleški
    COBISS.SI-ID - 700245

vir: Geologija. - ISSN 0016-7789 (vol. 43, 2, 2000, str. 219-221)

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