Structural meaning of the borehole LK-1/88 at Nadgorica by Ljubljana, Slovenia

Placer, Ladislav; Skaberne, Dragomir; Mlakar, Ivan

doi:10.5474/geologija.1999.014

Cited by 6 publications

(15 citation statements)

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“…Deep drilling at Cerkno (PLACER et al, 2000) confirmed the nappe structure with clear internal regularity. In the section across the Idrija deposit, the Trnovo Nappe is thrust for 32 km southwestward with respect to the Hru{ica Nappe, and the Hru{ica Nappe is shifted for 19 km with respect to the Sovi~ Thurst (PLACER, 1981). The length of shift has not been constructed for the Sovi~ Thrust, but is estimated to be in order of several kilometers.…”

Section: Trnovo Thrust Seriesmentioning

confidence: 99%

“…al., 1969;PLENI~AR et al, 1969;PLENI~AR et al, 1973;POL{AK, 1967;PREMRU, 1983;SAVI} & DOZET, 1985;[IKI} et al, 1969;[IKI} et al, 1972;[U{NJAR et al, 1970), of the compilation map Structural Model of Italy and Gravity Map, sheet 2 of scale 1 : 500.000 (BIGI et al, 1990) and Geologic Map of Friuli Venezia Giulia of scale 1 : 150.000 (CARULLI, 2006). In addition, all more important results from published works are considered (BI-ONDI} et al, 1997;BLA{KOVI}, 1999;COLIZZA et al, 1989;CUCCHI et al, 1989a,b;^AR & GOSPODARI~, 1983/84;JURKOV{EK et al, 1996;POLJAK & RI`NAR, 1996;MARIN~I} & MATI~EC, 1991;MATI~EC, 1994;MLAKAR, 1969;MLAKAR & PLACER, 2000;PERUZZA et al, 2002;PLACER & ^AR, 1997;PLACER, 1981PLACER, ,1982PLACER, , 1996PLACER, , 2005PLACER, , 2007PLACER, , 2008aPLACER, , 2008bPONTON, 2002). This paper is also based on published data from structural mapping of the motorway section Diva~a -Koper across the Istria-Friuli Underthrust Zone in years 1999 -2005, and Razdrto -Vipava, as well as the data from additional mapping of Razdrto -Senože~e road section, and of the seashore from Lazaret to Piran, and field inspections of key structural localities in the region between the Southern Alps and Velebit Mts.…”

Section: Tectonic Structurementioning

confidence: 99%

See 1 more Smart Citation

The bases for understanding of the NW Dinarides and Istria Peninsula tectonics

Placer¹,

Vrabec²,

Celarc³

2010

Geologija

Self Cite

103

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Section: Trnovo Thrust Seriesmentioning

confidence: 99%

Section: Tectonic Structurementioning

confidence: 99%

The bases for understanding of the NW Dinarides and Istria Peninsula tectonics

Placer¹,

Vrabec²,

Celarc³

2010

Geologija

Self Cite

103

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“…rock shelters at Veli Badin, for sizes see Table 1), which partly resemble cave entrances, but in the paper there are examples of describing overhangs on limestone-flysch contacts as rock shelters. PlaceR et al (2011) defined three types of rock shelters in Slovenian Istria: corrosion-freeze thaw type (e.g. caverns of Veli Badin), structural-tectonic type (overhang that represents a small thrust) and litologic-facial type (overhang, which is a result of differential weathering on a limestone-flysch contact).…”

Section: Characteristics Of Rock Shelters In Slovenian Istriamentioning

confidence: 99%

Rock shelters in Slovenian Istria as a potential for the development of geotourism in the region

Ozis¹,

Trpin²,

Šmuc³

2014

Geologija

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Geotourism is a special form of tourism which focuses on visiting geological and geomorphological sites. In the article we discuss the basic terms regarding geotourism, geodiversity and geoconservation, and then present the main features of rock shelters, i.e. landforms whose formation has not yet been elucidated. In our opinion rock shelters in Slovenian Istria have a potential to become sites for geotourism. We evaluated the geotourism potential of five rock shelter locations: Veli Badin, Štrkljevica, Mi{ja pe~, Stena and Kav~i~. The results of the evaluation show that three of the chosen rock shelter locations have a potential to develop as geotourist sites. Research confirmed our assumptions that the lack of scientific knowledge about rock shelters is a weakness from the geotourist point of view. Beside more detailed research on rock shelters, other activities, e.g. management of the sites, creating tourist activities, information material etc. are also needed if we want rock shelters to become geotourist sites in the future. Izvle~ekGeoturizem je posebna oblika turizma, ki se osredoto~a na obiskovanje geolo{kih in geomorfolo{kih naravnih znamenitosti. V ~lanku najprej predstavimo glavne pojme, ki se ti~ejo geoturizma, geodiverzitete in ohranjanja geo-dedi{~ine, nato pa se osredoto~imo na spodmole -reliefne oblike, katerih nastanek zaenkrat {e ni pojasnjen. Po na{em mnenju imajo spodmoli v Slovenski Istri potencial, da se razvijejo kot geoturisti~ne znamenitosti. Ovrednotili smo geoturisti~ni potencial petih lokacij spodmolov: Veli Badin, Štrkljevica, Mi{ja pe~, Stena in Kav~i~. Rezultati ocenjevanja so pokazali, da imajo tri lokacije potencial, da se razvijejo kot geoturisti~ne znamenitosti. Z raziskavo smo potrdili na{e domneve, da je z geoturisti~nega vidika pomanjkanje znanja o spodmolih slabost. Poleg bolj poglobljenih raziskav o spodmolih bodo potrebne tudi druge aktivnosti, npr. upravljanje z lokacijami, nudenje turisti~nih aktivnosti, izdelava informacijskega materiala o spodmolih itd., ~e želimo, da spodmoli v prihodnosti postanejo lokacije geoturisti~nega obiska.

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“…e karst area of south-western Slovenia belongs to the Dinaric Mountains, which tectonically (see Fig. 3) are a part of the External Dinarides (Placer 1981). e main area is on the Hrušica thrust sheet but part of Visoki kras (Trnovski gozd and Banjščica) belongs to the Trnovo thrust sheet (Placer 1999).…”

Section: Geology and Geomorphology Of The Dinarski Krasmentioning

confidence: 99%

Palaeomagnetism and Magnetostratigraphy of Karst Sediments in Slovenia

Hajna¹,

Mihevec²,

Pruner³

et al. 2008

Carsologica

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FOREWORD is book reports on the ten years long collaboration of theSlovene Karst Research Institute ZRC SAZU at Postojna with the Institute of Geology, Academy of Sciences of the Czech Republic at Praha (Prof. Pavel Bosak). e last institution has taken 2007 samples of sediments in the 21 profiles of the Slovene Dinaric and Alpine karst and determined their palaeomagnetism and magnetostratigraphy. e oldest sample found in them with the age from about 1.8 to more than 5.4 Ma indicated the surprising age of a cave near the Adriatic seashore. is is the time of the upper Miocene! Toward NE of the Slovene Dinaric Karst this age is diminishing but is still 0.78 Ma in the Postojnska jama. In one of the three researched high Alpine caves in the northern Slovenia this age is between 1.2 and 5.0 Ma.e study proved that the cave sediments represent a good tool for the reconstruction of the landscape evolution and tectonic regime in different karst regions. In collaboration with the team from Bohemia, the Slovene scientists added the results of research in many natural sciences on the Slovene caves and karst regions, already published or not yet published in the Slovenian and in the foreign literature. is is why this monograph on the Slovene karst caves and Slovene karst gives many new information. e famous French speleologist E. Martel in his book Les Abîmes in the year 1894 confirms the reputation of the Slovene Dinaric region Kras (Karst) by naming it "the classical karst" as here investigations of hydrology and caves started. e present book has repeated this reputation.Research in the Slovene caves contributed also to the improvement of the techniques of sampling for high resolution approach of fine cave sediments with dense sample spacing.e book is therefore important also for technology of sampling and for applying the palaeomagnetism and magnetostratigraphy for the karst sediments.

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Structural meaning of the borehole LK-1/88 at Nadgorica by Ljubljana, Slovenia

Cited by 6 publications

References 0 publications

The bases for understanding of the NW Dinarides and Istria Peninsula tectonics

The bases for understanding of the NW Dinarides and Istria Peninsula tectonics

Rock shelters in Slovenian Istria as a potential for the development of geotourism in the region

Palaeomagnetism and Magnetostratigraphy of Karst Sediments in Slovenia

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