Development of a Lithocodium (syn. Bacinella irregularis)-reef-mound- A patch reef within Middle Aptian lagoonal limestone sequence near Nova Gorica (Sabotin Mountain, W-Slovenia)

Koch, Roman; Moussavian, Esmail; Ogorelec, Bojan; Skaberne, Dragomir; Bucur, Ioan I.

doi:10.5474/geologija.2002.006

Cited by 21 publications

(27 citation statements)

References 12 publications

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“…Med grebeni, ki so se s prekinitvami vlekli {e v Suho Krajino in preko Gorjancev v Liko na Hrva{ko (veli} et al, 2002) so se odlagale medgrebenske bre~e ter plastoviti apnenci s hidrozojem Cladocoropsic mirabilis. Za zgornji malm (kimmeridgij in tithonij) so zopet zna~ilni oolitni in biomikritni apnenci z al gama Clypeina jurassica in Salpingoporella annulata (Buser, 1979b; strohMenGer & dozet, 1990) ter z aberantnimi tintinidami (ker~Mar, 1961). Med foraminife rami 25 Mikrofacies mezozojskih karbonatnih kamnin Slovenije so ugotovljene troholine (Trocholina alpina in T. elongata), Protopeneroplis striata, Pfenderina salernitana, Kurnubia palestinensis, K. jurassica in Nautiloculina oolithica (šriBar, lj.…”

Section: Dinarska Karbonatna Plo{~aunclassified

“…For the Upper Malm (Kimmeridgian and Tithonian) are again characteristic oolitic and biomicritic limestones with algae Clypeina jurassica and Salpingoporella annulata (Buser, 1979b;strohMenGer & dozet, 1990), and with aberrant tintinnidas (ker~Mar, 1961). Among foraminifers the trocholinas (Trocholina alpina in T. elongata), Protopeneroplis striata, Pfenderina salernitana, Kurnubia palestinensis, K. jurassica in Nautiloculina oolithica were recognized (šriBar lj.…”

Section: Dinaric Carbonate Platformmentioning

confidence: 99%

“…17 -Laze pri Sevnici (oGorelec & dozet, 1997), 18 -Kobla (Buser & oGorelec, 2008 roži~, 2005), 19 -Batognica pri Krnu (BaBi}, 1980, 20 -Julijske Alpe -Trenta (jurkov{ek et al, ), 21 -Mangart (jurkov{ek et al, 1990šMuc, 2005), 22 -Bovec (oGorelec et al, 2006), 23 -Zalilog (BaBi} & zuPani~, 1978), 24 -Delnice (dozet & šriBar, 1991), 25 -Podhosta, Ko~evski Rog (orehek & oGorelec, 1985, 26 -Ko~evsko (dozet, 1990), 27 -Trnovo (koch, 1988koch et al, 1989;koch & oGorelec, 1990), 28 -Logatec (šriBar, 1979, 29 -Slovenski vrh - Ko~evje (turn{ek et al, 1992), 30 -Dutovlje (koch & oGorelec, 1987), 31 -Nanos (koch, 1977 koch et al, 1998;šriBar lu., 1995), 32 -Nanos -Nadrt ( jurkov{ek, 2008), 42 -Komen (oGorelec et al, 1987a, 1996bjurkov{ek et al, 1996;jurkov{ek & kolar-jurkov{ek, 2007), 43 -Senože~e (Pleni~ar & jurkov{ek, 1996Pleni~ar, 2005), 44 -Kozina (delwalle & Buser, 1990), 45 -^ebulovica (oGo relec et al, 2001), 46 -Kras -K/T meja (K/T boundary) (oGorelec et al, 1995(oGorelec et al, , 2007hansen et al, 1995;PuGliese et al, 1995;riccaMBoni, 2005), 47 -Dolenja vas (droBne et al, 1988, 1995), 48 -Gori{ka Brda (šriBar, 1965, 49 -Bohor, Kr{ko (Buser et al, 1982a), 50 -Podbrdo -Zalilog (BaBi} & zuPani~, 1978), 51 -Banj{ka planota (turn{ek & Buser, 1976), 52 -Doblar -vol~anski apnenec (Vol~e limestone) (oGorelec et al, 1976, 1987b), 53 -Bovec (ku{~er et al, 1974radoi~i} & Buser, 2004) 1969, 1972, 1997; turn{ek ...…”

Section: Dinarska Karbonatna Plo{~amentioning

confidence: 99%

“…Na Krasu je taka okopnitev nakazana z emerzijsko bre~o na meji med Brsko in Povirsko formacijo (sl. 19) oziroma na meji med aptijem in albijem jurkov{ek, 2008koch & oGorelec, 1987). Apnenec od valanginijske pa vse do albijske starosti je pogosto dolomitiziran, delno ali v popolnosti; dolomitizacija ima poznodiagenetski zna~aj.…”

unclassified

“…Schematic presentation of lithologic development of Jurassic and Cretaceous carbonate rocks in Slovenia with the position of lithostratigraphic sections and their reference data. 1 -Jugorje -Gorjanci (orehek & oGorelec, 1980/81), 2 -Prezid, Ko~evsko (dozet & šriBar, 1981, dozet, 1992a, 3 -Mala gora -Kompolje (strohMenGer & dozet, 1990, strohMenGer et al, 1987), 4 -Bela Krajina, Ko~evski Rog (dozet, 1996, 5 -Južna Slovenija (Ko~evska gora, Goteni{ka gora, dozet, 1990c), 6 -Krka -Mali Korinj (strohMenGer & dozet, 1990, dozet, 1993 (turn{ek, 1966, 1969, 1972, 1997; turn{ek et al, 1981),17 -Laze pri Sevnici (oGorelec & dozet, 1997), 18 -Kobla (Buser & oGorelec, 2008 roži~, 2005), 19 -Batognica pri Krnu (BaBi}, 1980, 20 -Julijske Alpe -Trenta (jurkov{ek et al, ), 21 -Mangart (jurkov{ek et al, 1990šMuc, 2005), 22 -Bovec (oGorelec et al, 2006), 23 -Zalilog (BaBi} & zuPani~, 1978), 24 -Delnice (dozet & šriBar, 1991), 25 -Podhosta, Ko~evski Rog (orehek & oGorelec, 1985, 26 -Ko~evsko (dozet, 1990), 27 -Trnovo (koch, 1988koch et al, 1989;koch & oGorelec, 1990), 28 -Logatec (šriBar, 1979, 29 -Slovenski vrh - Ko~evje (turn{ek et al, 1992), 30 -Dutovlje (koch & oGorelec, 1987), 31 -Nanos (koch, 1977 koch et al, 1998;šriBar lu., 1995), 32 -Nanos -Nadrt ( jurkov{ek, 2008), 42 -Komen (oGorelec et al, 1987a, 1996bjurkov{ek et al, 1996;jurkov{ek & kolar-jurkov{ek, 2007), 43 -Senože~e (Pleni~ar & jurkov{ek, 1996Pleni~ar, 2005), 44 -Kozina (delwalle & Buser, 1990), 45 -^ebulovica (oGo relec et al, 2001), 46 -Kras -K/T meja (K/T boundary) (oGorelec et al, 1995(oGorelec et al, , 2007hansen et al, 1995;PuGliese et al, 1995;riccaMBoni, 2005), 47 -Dolenja vas (droBne et al, 1988…”

mentioning

confidence: 99%

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Microfacies of Mesozoic Carbonate

Ogorelec¹

2011

Geologija

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Steklo tanko, kos apnenca, tanek snop svetlobe -~arovnija,nam pri~ara morje plitvo, plažo, ocean globine. Izvle~ekKarbonatne kamnine mezozojske starosti so v Sloveniji precej raz{irjene, saj zavzemajo kar okrog 40 % njenega ozemlja, njihova celotna skladovnica pa je debela preko 5000 metrov. V mikrofaciesu apnencev in dolomitov prepoznamo skoraj vse strukturne tipe, saj so nastajali v razli~nih sedimentacijskih okoljih, zna~ilnih za karbonatne kamnine, tako v odprtih in zati{nih delih karbonatnega {elfa, lagunah in na obrežnih ravnicah, na razli~nih vrstah grebenov, pregibih in v bazenu. Ve~krat so karbonatno sedimentacijo spremljali tudi dotoki terigenega materiala in produkti vulkanskih aktivnosti. Med diagenetskimi procesi raziskanih karbonatnih kamnin imata najve~ji obseg dolomitizacija in okremenitev.V prispevku je predstavljenih 250 mikroskopskih posnetkov zna~ilnih apnencev in dolomitov s slovenskega prostora. V uvodnem delu, v katerem so za orientacijo dodani shematski litostratigrafski stolpci, je na kratko predstavljen geolo{ki razvoj karbonatnih kamnin. Zaradi celostnega prikaza »karbonatnega obdobja« so poleg mezozojskih plasti v pregledu zajeti tudi zgornjepermski apnenci in dolomiti. AbstractCarbonate rocks of Mesozoic age are widespread in Slovenia where they consitute about 40 % of its territory, and attaining total thickness of more than 5000 metres . With respect to microfacies almost all structure types can be recognized, the limestones and dolomites being formed in various sedimentary environments, such as in open and in restricted parts of carbonate shelf, in lagoons and on coastal plains, in different types of reefs, on slopes and in the basin. Carbonate sedimentation was often accompanied also by the supply of terrigenous material and products of volcanic activity. Among diagenetic processes in investigated carbonate rocks the most extensive are dolomitization and silicification.In the present text 250 microscopic photographs of characteristic limestones and dolomites from Slovenian territory are assembled. In the introductory part, to which for orientation schematic stratigraphic columns are added, the geologic development od these carbonate rocks is briefly outlined. For the sake of completeness in presenting the »carbonate era« in the overview, Upper Permian limestones and dolomites are also described next to Mesozoic beds. Carbonate rocks are born ... (James N.P., 1979) Ob 50. obletnici izida klasifikacije karbonatnih kamnin (Folk 1962, Dunham 1962, Ham (ed.) 1962. UVODKarbonatne kamnine mezozojske starosti gradijo okrog 40 % slovenskega ozemlja (Buser & koMac, 2002). V tej, preko 5.000 metrov debeli skladovnici apnencev in dolomitov, ki jih le mestoma prekinjajo klasti~ne sedimentne kamnine, vulkaniti in piroklastiti, zasledimo skoraj vse facialne razvoje, zna~ilne tako za plitvomorska karbonatna okolja kot za globljemorska okolja. Na majhnem prostoru je razvito celotno zaporedje sedimentnih kamnin v stratigrafskem razponu od devona do kvartarja. Ta raznolikost je v precej{nji meri p...

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Section: Dinarska Karbonatna Plo{~aunclassified

Section: Dinaric Carbonate Platformmentioning

confidence: 99%