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Zgornjetriasne in spodnjejurske plasti na območju Podutika pri Ljubljani = Upper Triassic and Lower Jurassic beds in the Podutik area near Ljubljana (Slovenia)Novak, MatevžNa območju Podutika pri Ljubljani je v noriju in retiju v zelo plitvem lagunskem okolju zaprtega šelfa na Dinarski karbonatni platformi nastajal glavni dolomit, na severnem robu platforme pa na ... plitvem odprtem šelfu dachsteinski apnenec. Zaradi pomanjkanja fosilov retijska stopnja ni ločena odnorijske. Meja med trisom in juro je zaznamovana v glavnem s postopnim litološkim prehodom.Source: Geologija. - ISSN 0016-7789 (Knj. 46, [št.] 1, 2003, str. 65-74)Type of material - article, component partPublish date - 2003Language - slovenianCOBISS.SI-ID - 966229
Author
Novak, Matevž
Topics
Dinaridi |
trias |
jura |
stratigrafija |
sedimentne kamnine |
apnenec |
dolomit |
Ljubljana |
Podutik
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Database name | Field | Year |
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Links to authors' personal bibliographies | Links to information on researchers in the SICRIS system |
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Novak, Matevž | 21384 |
Source: Personal bibliographies
and: SICRIS
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