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Geološka karta Zgornje Vipavske doline med Velikim poljem na Krasu in Debelo steno na Nanosu : diplomsko delo = geological map of Upper Vipava valley between Veliko polje on Kras and debela stena na Nanosu : diploma thesisBizjak, Jaka, 1986-V diplomski nalogi sem izdelal detajlno geološko karto območja Zgornje Vipavske doline. Ozemlje pripada tektonski enoti Zunanjih Dinaridov, natančneje Snežniško-hrušiškemu pokrovu ter Komenski ... narivni grudi. Najstarejše kamnine na območju se nahajajo v apnenčastih ostenjih Nanosa. Tu gre za bioklastične apnence, algalno-foraminiferno-bioklastične apnence ter rudistne apnence campanijske in spodnje maastrichtijske starosti. Te predstavljajo kamnine Hrušiškega pokrova, ki so narinjene na mlajše siliciklastične flišne kamnine. Na območju Krasa izdanja liburnijska formacija. Bituminozni apnenci Kozinskega faciesa, ki so člen liburnijske formacije, se stikajo z bazalnimi brečami in konglomerati fliša. Liburnijska formacija je maastrichtijske in paleocenske starosti. Na bazalnih konglomeratih in brečah so odložene sp. eocenske flišne kamnine. Gre za menjavanje plasti peščenjakov, laporovcev, muljevcev ter kalciturbiditnih plasti. Ti so sestavljeni iz karbonatnih breč ali konglomeratov v bazi iz apnencev oziroma kalkarenitov, zaporedje pa se zaključi z laporovci. Paleogeografsko je bilo ozemlje v kredi - na Krasu pa še v začetku paleogena - del Dinarske karbonatne platforme, v eocenu pa se je poglobilo v predgorski bazen s flišno sedimentacijo. Najmlajše kamnine oziroma sedimente predstavljajo kvartarni grušči, ki so ponekod sprijeti v brečo. Ti vsebujejo klaste krednih apnencev in flišnih peščenjakov, ki so nastale kot posledica erozije in gravitacijskih tokov Nanoškega JZ pobočja. Kartirano območje sestoji iz treh tektonskih enot. Na SV so kredni apnenci Hrušiškega pokrova narinjeni na eocenske siliciklastične flišne kamnine Snežniškega pokrova, te pa so narinjene na eocenske kamnine Komenske narivne grude. Plasti generalno vpadajo proti SV z različnimi nakloni, od 40° do 80°. Čez ozemlje poteka večja dinarsko usmerjena cona deformiranih kamnin, s smerjo slemenitve SZ % JV. Po mnenju nekaterih avtorjev gre za prelomno cono Vipavskega preloma, vendar sam nisem našel nobenih dokazov, ki bi to potrjevali. Cono bi lahko interpretirali kot narivnico Snežniškega pokrova.Type of material - undergraduate thesis ; adult, seriousPublication and manufacture - Ljubljana : [J. Bizjak], 2015Language - slovenianCOBISS.SI-ID - 1232990
Author
Bizjak, Jaka, 1986-
Other authors
Rožič, Boštjan, 1974- |
Popit, Tomislav
Topics
geologija |
kartiranje |
Zgornja Vipavska dolina |
Veliko polje |
Debela stena |
Kras |
Nanos
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Library/institution |
City | Acronym | For loan | Other holdings |
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NTF, Department of Geology, Ljubljana | Ljubljana | NTFGEO |
outside loan 1 cop.
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DRS, in which the journal is indexed
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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Bizjak, Jaka, 1986- | ![]() |
Rožič, Boštjan, 1974- | 23426 |
Popit, Tomislav | 23971 |
Source: Personal bibliographies
and: SICRIS
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