TY  - JOUR
AU  - Petrović, Aleksandar S.
AU  - Nikolić, Dragana
AU  - Trnavac-Bogdanović, Dušica
AU  - Carević, Ivana
PY  - 2020
UR  - https://gery.gef.bg.ac.rs/handle/123456789/1071
AB  - Protection and promotion of geoheritage has been changing and improving in recent decades, in line with the growing research in this field. Some research papers specifically study geomorphological geoheritage and introduce a special term - geomorphosite. Karst geomorphosites present specific objects of geomorphological heritage. On Kucaj and Beljanica mountains there is the largest karst area in Serbia. The purpose of this paper is to select and evaluate the scientific value of karst geomorphosites of Kucaj and Beljanica. More than one hundred karst geomorphosites were analyzed. In order to achieve more adequate coverage and representation, they were grouped into 25 geomorphotypes in three major geomorphological components of the investigated area. The results of this analysis highlighted the most important natural potentials of this area for establishing a karst-based geopark. More than 20 geomorphotypes have a positive recommendation index, which provides a good basis for further geotourism analysis.
PB  - Karst Research Inst Zrc Sazu, Postojna
T2  - Acta Carsologica
T1  - Assessment of karst geomorphosites on Kucaj and Beljanica mountains as a resource for the development of karst-based geopark
VL  - 49
IS  - 2-3
SP  - 179
EP  - 190
DO  - 10.3986/ac.v49i2-3.8748
UR  - https://hdl.handle.net/21.15107/rcub_gery_1071
ER  - 

@article{
author = "Petrović, Aleksandar S. and Nikolić, Dragana and Trnavac-Bogdanović, Dušica and Carević, Ivana",
year = "2020",
abstract = "Protection and promotion of geoheritage has been changing and improving in recent decades, in line with the growing research in this field. Some research papers specifically study geomorphological geoheritage and introduce a special term - geomorphosite. Karst geomorphosites present specific objects of geomorphological heritage. On Kucaj and Beljanica mountains there is the largest karst area in Serbia. The purpose of this paper is to select and evaluate the scientific value of karst geomorphosites of Kucaj and Beljanica. More than one hundred karst geomorphosites were analyzed. In order to achieve more adequate coverage and representation, they were grouped into 25 geomorphotypes in three major geomorphological components of the investigated area. The results of this analysis highlighted the most important natural potentials of this area for establishing a karst-based geopark. More than 20 geomorphotypes have a positive recommendation index, which provides a good basis for further geotourism analysis.",
publisher = "Karst Research Inst Zrc Sazu, Postojna",
journal = "Acta Carsologica",
title = "Assessment of karst geomorphosites on Kucaj and Beljanica mountains as a resource for the development of karst-based geopark",
volume = "49",
number = "2-3",
pages = "179-190",
doi = "10.3986/ac.v49i2-3.8748",
url = "https://hdl.handle.net/21.15107/rcub_gery_1071"
}

Petrović, A. S., Nikolić, D., Trnavac-Bogdanović, D.,& Carević, I.. (2020). Assessment of karst geomorphosites on Kucaj and Beljanica mountains as a resource for the development of karst-based geopark. in Acta Carsologica
Karst Research Inst Zrc Sazu, Postojna., 49(2-3), 179-190.
https://doi.org/10.3986/ac.v49i2-3.8748
https://hdl.handle.net/21.15107/rcub_gery_1071

Petrović AS, Nikolić D, Trnavac-Bogdanović D, Carević I. Assessment of karst geomorphosites on Kucaj and Beljanica mountains as a resource for the development of karst-based geopark. in Acta Carsologica. 2020;49(2-3):179-190.
doi:10.3986/ac.v49i2-3.8748
https://hdl.handle.net/21.15107/rcub_gery_1071 .

Petrović, Aleksandar S., Nikolić, Dragana, Trnavac-Bogdanović, Dušica, Carević, Ivana, "Assessment of karst geomorphosites on Kucaj and Beljanica mountains as a resource for the development of karst-based geopark" in Acta Carsologica, 49, no. 2-3 (2020):179-190,
https://doi.org/10.3986/ac.v49i2-3.8748 .,
https://hdl.handle.net/21.15107/rcub_gery_1071 .

TY  - THES
AU  - Petrović, Aleksandar S.
PY  - 2015
UR  - http://nardus.mpn.gov.rs/handle/123456789/5755
UR  - http://eteze.bg.ac.rs/application/showtheses?thesesId=3128
UR  - https://fedorabg.bg.ac.rs/fedora/get/o:11431/bdef:Content/download
UR  - http://vbs.rs/scripts/cobiss?command=DISPLAY&base=70036&RID=47561487
UR  - https://gery.gef.bg.ac.rs/handle/123456789/1101
AB  - The analysis of basic morphological characteristics of the valleys in karst of the Serbian Carpatho-Balkanides showed the noticeable morphological differences (polymorphism). Polymorphism is a consequence of the influence of modifiers during the process of valley origin. The aim of the dissertation is to explain the causality of this influence within the case study of valleys in karst of the Serbian Carpatho-Balkanides, as well as to determine the dominant modifiers. The qualitative analyses are conducted on 2717 valleys and quantitative analyses on selected samples of 910 valleys. The comparative analysis of all the obtained results showed that several modifiers are dominant. None of these modifiers operates independently, but the combined effect of several dominant modifiers is evident. Dominant modifiers which lead to the polymorphism of valleys in karst of the Serbian Carpatho-Balkanides are: the contact of carbonate and non-carbonate rocks, precipitation, hydrological function of the valleys, inclinations of the valley floor and of the terrain in which the valley is incised, the thickness of carbonate rocks, fissure permeability and the intensity of karst process.
AB  - Analizom osnovnih morfoloških karakteristika dolina u krasu Karpato-balkanida Srbije utvrđeno je postojanje njihove morfološke raznolikosti (polimorfije). Polimorfija dolina u krasu se javlja kao posledica uticaja pojedinih modifikatora tokom procesa nastanka dolina. Cilj disertacije je objašnjavanje uzročnosti i zakonitosti uticaja modifikatora na pojavu polimorfije dolina u krasu Karpato- balkanida Srbije i određivanje dominantnih modifikatora polimorfije dolina u krasu. Istraživanje je sprovedeno na 2717 dolina (kvalitativna analiza), odnosno, na odabranom uzorku od 910 dolina (kvantitativna analiza). Komparativnom analizom svih dobijenih rezultata tokom istraživanja zaključeno je da u objašnjenju morfološke raznolikosti dolina u krasu Karpato-balkanida Srbije dominira nekoliko modifikatora. Ni jedan od ovih modifikatora ne deluje samostalno, već je evidentan zajednički uticaj više dominantnih modifikatora. Dominantni modifikatori koji utiču na polimorfiju dolina u krasu Karpato-balkanida Srbije su: kontakt karbonata sa nekarbonatnim stenama, padavine, hidrološka funkcija dolina, nagib dna doline i nagib reljefa u koji je dolina usečena, debljina karbonatne mase, pukotinska poroznost i intenzitet kraškog procesa.
PB  - Univerzitet u Beogradu, Geografski fakultet
T1  - Uticaj modifikatora na polimorfiju dolina u krasu Karpato-balkanida Srbije
T1  - The influence of modifiers on the polimorphy of valley in karst of the serbian carpatho-balkanides.
UR  - https://hdl.handle.net/21.15107/rcub_nardus_5755
ER  - 

@phdthesis{
author = "Petrović, Aleksandar S.",
year = "2015",
abstract = "The analysis of basic morphological characteristics of the valleys in karst of the Serbian Carpatho-Balkanides showed the noticeable morphological differences (polymorphism). Polymorphism is a consequence of the influence of modifiers during the process of valley origin. The aim of the dissertation is to explain the causality of this influence within the case study of valleys in karst of the Serbian Carpatho-Balkanides, as well as to determine the dominant modifiers. The qualitative analyses are conducted on 2717 valleys and quantitative analyses on selected samples of 910 valleys. The comparative analysis of all the obtained results showed that several modifiers are dominant. None of these modifiers operates independently, but the combined effect of several dominant modifiers is evident. Dominant modifiers which lead to the polymorphism of valleys in karst of the Serbian Carpatho-Balkanides are: the contact of carbonate and non-carbonate rocks, precipitation, hydrological function of the valleys, inclinations of the valley floor and of the terrain in which the valley is incised, the thickness of carbonate rocks, fissure permeability and the intensity of karst process., Analizom osnovnih morfoloških karakteristika dolina u krasu Karpato-balkanida Srbije utvrđeno je postojanje njihove morfološke raznolikosti (polimorfije). Polimorfija dolina u krasu se javlja kao posledica uticaja pojedinih modifikatora tokom procesa nastanka dolina. Cilj disertacije je objašnjavanje uzročnosti i zakonitosti uticaja modifikatora na pojavu polimorfije dolina u krasu Karpato- balkanida Srbije i određivanje dominantnih modifikatora polimorfije dolina u krasu. Istraživanje je sprovedeno na 2717 dolina (kvalitativna analiza), odnosno, na odabranom uzorku od 910 dolina (kvantitativna analiza). Komparativnom analizom svih dobijenih rezultata tokom istraživanja zaključeno je da u objašnjenju morfološke raznolikosti dolina u krasu Karpato-balkanida Srbije dominira nekoliko modifikatora. Ni jedan od ovih modifikatora ne deluje samostalno, već je evidentan zajednički uticaj više dominantnih modifikatora. Dominantni modifikatori koji utiču na polimorfiju dolina u krasu Karpato-balkanida Srbije su: kontakt karbonata sa nekarbonatnim stenama, padavine, hidrološka funkcija dolina, nagib dna doline i nagib reljefa u koji je dolina usečena, debljina karbonatne mase, pukotinska poroznost i intenzitet kraškog procesa.",
publisher = "Univerzitet u Beogradu, Geografski fakultet",
title = "Uticaj modifikatora na polimorfiju dolina u krasu Karpato-balkanida Srbije, The influence of modifiers on the polimorphy of valley in karst of the serbian carpatho-balkanides.",
url = "https://hdl.handle.net/21.15107/rcub_nardus_5755"
}

Petrović, A. S.. (2015). Uticaj modifikatora na polimorfiju dolina u krasu Karpato-balkanida Srbije. 
Univerzitet u Beogradu, Geografski fakultet..
https://hdl.handle.net/21.15107/rcub_nardus_5755

Petrović AS. Uticaj modifikatora na polimorfiju dolina u krasu Karpato-balkanida Srbije. 2015;.
https://hdl.handle.net/21.15107/rcub_nardus_5755 .

Petrović, Aleksandar S., "Uticaj modifikatora na polimorfiju dolina u krasu Karpato-balkanida Srbije" (2015),
https://hdl.handle.net/21.15107/rcub_nardus_5755 .

TY  - JOUR
AU  - Petrović, Aleksandar S.
AU  - Carević, Ivana
PY  - 2015
UR  - https://gery.gef.bg.ac.rs/handle/123456789/670
AB  - The paper deals with the description of Samar natural bridge and collapse valley of Ravna River in eastern Serbia aiming to suggest an interpretation of their origin and development, in relationship with lithological and tectonic conditions, karst processes, and petrological analyses. In this study we present the geological setting, detailed morphology and hypothesis on the genesis of these karst landforms. The relationship between surface karst development and the geology is considerably acknowledged. The major contribution of the paper is to propose a framework for considering how recrystallization of limestone can affect the weathering potential of karst landforms and to introduce a term collapse valley. Finally, this study shows that the weathering potencial of the Samar natural bridge is decreased concerning the diagenetic changes these limestones underwent.
PB  - Zalozba Z R C
T2  - Acta Carsologica
T1  - Geological influence on the formation of samar natural bridge and collapse valley of ravna river from the ne kucaj mountains (carpatho-balkanides, eastern Serbia)
VL  - 44
IS  - 1
SP  - 37
EP  - 46
DO  - 10.3986/ac.v44i1.898
UR  - https://hdl.handle.net/21.15107/rcub_gery_670
ER  - 

@article{
author = "Petrović, Aleksandar S. and Carević, Ivana",
year = "2015",
abstract = "The paper deals with the description of Samar natural bridge and collapse valley of Ravna River in eastern Serbia aiming to suggest an interpretation of their origin and development, in relationship with lithological and tectonic conditions, karst processes, and petrological analyses. In this study we present the geological setting, detailed morphology and hypothesis on the genesis of these karst landforms. The relationship between surface karst development and the geology is considerably acknowledged. The major contribution of the paper is to propose a framework for considering how recrystallization of limestone can affect the weathering potential of karst landforms and to introduce a term collapse valley. Finally, this study shows that the weathering potencial of the Samar natural bridge is decreased concerning the diagenetic changes these limestones underwent.",
publisher = "Zalozba Z R C",
journal = "Acta Carsologica",
title = "Geological influence on the formation of samar natural bridge and collapse valley of ravna river from the ne kucaj mountains (carpatho-balkanides, eastern Serbia)",
volume = "44",
number = "1",
pages = "37-46",
doi = "10.3986/ac.v44i1.898",
url = "https://hdl.handle.net/21.15107/rcub_gery_670"
}

Petrović, A. S.,& Carević, I.. (2015). Geological influence on the formation of samar natural bridge and collapse valley of ravna river from the ne kucaj mountains (carpatho-balkanides, eastern Serbia). in Acta Carsologica
Zalozba Z R C., 44(1), 37-46.
https://doi.org/10.3986/ac.v44i1.898
https://hdl.handle.net/21.15107/rcub_gery_670

Petrović AS, Carević I. Geological influence on the formation of samar natural bridge and collapse valley of ravna river from the ne kucaj mountains (carpatho-balkanides, eastern Serbia). in Acta Carsologica. 2015;44(1):37-46.
doi:10.3986/ac.v44i1.898
https://hdl.handle.net/21.15107/rcub_gery_670 .

Petrović, Aleksandar S., Carević, Ivana, "Geological influence on the formation of samar natural bridge and collapse valley of ravna river from the ne kucaj mountains (carpatho-balkanides, eastern Serbia)" in Acta Carsologica, 44, no. 1 (2015):37-46,
https://doi.org/10.3986/ac.v44i1.898 .,
https://hdl.handle.net/21.15107/rcub_gery_670 .

TY  - JOUR
AU  - Petrović, Aleksandar S.
PY  - 2014
UR  - https://gery.gef.bg.ac.rs/handle/123456789/646
AB  - The Zijovo Range belongs to the Prokletije Mountains of Montenegro and is located in the extreme southeast, on the border with Albania. Glacial processes were intensively active in this range during the Pleistocene. This is indicated by erosive and accumulative glacial features of relief that have been preserved due to the favorable geologic structure. The glacial maximum in the Zijovo Range is characterized by a unique glacier on the entire area of the range. Preglacial relief prevented the formation of a typical icecap glacier. Due to drainage of the central glacial mass in the direction of the preglacial valleys, there was a transection glacier in the central, northern, and northwestern parts, and an icefield glacier in the eastern and southeastern parts of the Zijovo Range. These glaciers covered an area of 180 km during the glacial maximum.
PB  - Ljubljana: Geografski inštitut Antona Melika ZRC SAZU
T2  - Acta Geographica Slovenica - Geografski zbornik
T1  - A reconstruction of the pleistocene glacial maximum in the Zijovo range (Prokletije mountains, Montenegro)
VL  - 54
IS  - 2
SP  - 255
EP  - 269
DO  - 10.3986/AGS54202
UR  - https://hdl.handle.net/21.15107/rcub_gery_646
ER  - 

@article{
author = "Petrović, Aleksandar S.",
year = "2014",
abstract = "The Zijovo Range belongs to the Prokletije Mountains of Montenegro and is located in the extreme southeast, on the border with Albania. Glacial processes were intensively active in this range during the Pleistocene. This is indicated by erosive and accumulative glacial features of relief that have been preserved due to the favorable geologic structure. The glacial maximum in the Zijovo Range is characterized by a unique glacier on the entire area of the range. Preglacial relief prevented the formation of a typical icecap glacier. Due to drainage of the central glacial mass in the direction of the preglacial valleys, there was a transection glacier in the central, northern, and northwestern parts, and an icefield glacier in the eastern and southeastern parts of the Zijovo Range. These glaciers covered an area of 180 km during the glacial maximum.",
publisher = "Ljubljana: Geografski inštitut Antona Melika ZRC SAZU",
journal = "Acta Geographica Slovenica - Geografski zbornik",
title = "A reconstruction of the pleistocene glacial maximum in the Zijovo range (Prokletije mountains, Montenegro)",
volume = "54",
number = "2",
pages = "255-269",
doi = "10.3986/AGS54202",
url = "https://hdl.handle.net/21.15107/rcub_gery_646"
}

Petrović, A. S.. (2014). A reconstruction of the pleistocene glacial maximum in the Zijovo range (Prokletije mountains, Montenegro). in Acta Geographica Slovenica - Geografski zbornik
Ljubljana: Geografski inštitut Antona Melika ZRC SAZU., 54(2), 255-269.
https://doi.org/10.3986/AGS54202
https://hdl.handle.net/21.15107/rcub_gery_646

Petrović AS. A reconstruction of the pleistocene glacial maximum in the Zijovo range (Prokletije mountains, Montenegro). in Acta Geographica Slovenica - Geografski zbornik. 2014;54(2):255-269.
doi:10.3986/AGS54202
https://hdl.handle.net/21.15107/rcub_gery_646 .

Petrović, Aleksandar S., "A reconstruction of the pleistocene glacial maximum in the Zijovo range (Prokletije mountains, Montenegro)" in Acta Geographica Slovenica - Geografski zbornik, 54, no. 2 (2014):255-269,
https://doi.org/10.3986/AGS54202 .,
https://hdl.handle.net/21.15107/rcub_gery_646 .

TY  - JOUR
AU  - Petrović, Aleksandar S.
AU  - Veselinović, Ratomir
PY  - 2012
UR  - https://gery.gef.bg.ac.rs/handle/123456789/527
AB  - The evolution of Gajina mlaka paleovalley from pre-karstic to current phase reveals the complexity of process of transformation of valleys in karst and formation of fluviokarst uvalas. The creation of river network and formation of the valley of Gajina mlaka are related to successive withdrawal of the Pontiac Sea. Predominance of karstic process over fluvial causes the transformation of fluvial morphology into karstic. The degree of transformation depends on relationship of the intensity between these two opposed processes. Karstification covers all parts of Gajina mlaka valley which are built in karst. Riverbeds are almost completely transformed and dolines are formed along them. In the parts of valleys with more significant lithologic differences, more complex tectonic relationships and different pre-karstic fluvial morphology, larger forms of relief are created by karstic process and they are called uvalas. According to the presented method of genesis and evolution of uvalas it can be concluded that they are clearly morphologically and genetically individualized karst landforms, which negates some contemporary opinions that exclude both the term and form uvala as karstic element of relief.
AB  - Evolucija paleodoline Gajina mlaka od prekraške do savremene faze otkriva složenost procesa transformacije dolina u krasu i nastanak fluvio-kraških uvala. Nastanak rečne mreže i stvaranje doline Gajina mlaka vezan je za sukcesivno povlačenje Pontiskog mora. Prevaga kraškog procesa nad fluvijalnim dovodi do transformacije fluvijane morfologije u krašku. Stepen transformacije zavisi od odnosa inteziteta ova dva suprostavljena procesa. Karstifikacija zahvata sve delove doline Gajina mlaka koji su izgrađeni u krečnjacima. Rečna korita su gotovo u potpunosti preoblikovana i duž njih se formiraju vrtače. U delovima dolina sa značajnijim litološkim razlikama, složenijim tektonskim odnosima i različitom prekraškom fluvijalnom morfologijom kraškim procesom izgrađuju se veći oblici reljefa - uvale. Iz prikazanog načina nastanka i evolucije uvala proističe da su one jasno morfološki i genetski individualisani kraški oblici, čime se negiraju pojedina savremena shvatanja koja isključuju i termin i oblik uvale kao kraškog elementa reljefa.
PB  - Beograd : Srpsko geografsko društvo
T2  - Glasnik Srpskog geografskog društva
T1  - The genesis and evolution of uvalas in Gajina mlaka paleovalley on the Kučaj mountains
T1  - Geneza i evolucija uvala u paleodolini Gajina mlaka na Kučaju
VL  - 92
IS  - 1
SP  - 91
EP  - 104
UR  - https://hdl.handle.net/21.15107/rcub_gery_527
ER  - 

@article{
author = "Petrović, Aleksandar S. and Veselinović, Ratomir",
year = "2012",
abstract = "The evolution of Gajina mlaka paleovalley from pre-karstic to current phase reveals the complexity of process of transformation of valleys in karst and formation of fluviokarst uvalas. The creation of river network and formation of the valley of Gajina mlaka are related to successive withdrawal of the Pontiac Sea. Predominance of karstic process over fluvial causes the transformation of fluvial morphology into karstic. The degree of transformation depends on relationship of the intensity between these two opposed processes. Karstification covers all parts of Gajina mlaka valley which are built in karst. Riverbeds are almost completely transformed and dolines are formed along them. In the parts of valleys with more significant lithologic differences, more complex tectonic relationships and different pre-karstic fluvial morphology, larger forms of relief are created by karstic process and they are called uvalas. According to the presented method of genesis and evolution of uvalas it can be concluded that they are clearly morphologically and genetically individualized karst landforms, which negates some contemporary opinions that exclude both the term and form uvala as karstic element of relief., Evolucija paleodoline Gajina mlaka od prekraške do savremene faze otkriva složenost procesa transformacije dolina u krasu i nastanak fluvio-kraških uvala. Nastanak rečne mreže i stvaranje doline Gajina mlaka vezan je za sukcesivno povlačenje Pontiskog mora. Prevaga kraškog procesa nad fluvijalnim dovodi do transformacije fluvijane morfologije u krašku. Stepen transformacije zavisi od odnosa inteziteta ova dva suprostavljena procesa. Karstifikacija zahvata sve delove doline Gajina mlaka koji su izgrađeni u krečnjacima. Rečna korita su gotovo u potpunosti preoblikovana i duž njih se formiraju vrtače. U delovima dolina sa značajnijim litološkim razlikama, složenijim tektonskim odnosima i različitom prekraškom fluvijalnom morfologijom kraškim procesom izgrađuju se veći oblici reljefa - uvale. Iz prikazanog načina nastanka i evolucije uvala proističe da su one jasno morfološki i genetski individualisani kraški oblici, čime se negiraju pojedina savremena shvatanja koja isključuju i termin i oblik uvale kao kraškog elementa reljefa.",
publisher = "Beograd : Srpsko geografsko društvo",
journal = "Glasnik Srpskog geografskog društva",
title = "The genesis and evolution of uvalas in Gajina mlaka paleovalley on the Kučaj mountains, Geneza i evolucija uvala u paleodolini Gajina mlaka na Kučaju",
volume = "92",
number = "1",
pages = "91-104",
url = "https://hdl.handle.net/21.15107/rcub_gery_527"
}

Petrović, A. S.,& Veselinović, R.. (2012). The genesis and evolution of uvalas in Gajina mlaka paleovalley on the Kučaj mountains. in Glasnik Srpskog geografskog društva
Beograd : Srpsko geografsko društvo., 92(1), 91-104.
https://hdl.handle.net/21.15107/rcub_gery_527

Petrović AS, Veselinović R. The genesis and evolution of uvalas in Gajina mlaka paleovalley on the Kučaj mountains. in Glasnik Srpskog geografskog društva. 2012;92(1):91-104.
https://hdl.handle.net/21.15107/rcub_gery_527 .

Petrović, Aleksandar S., Veselinović, Ratomir, "The genesis and evolution of uvalas in Gajina mlaka paleovalley on the Kučaj mountains" in Glasnik Srpskog geografskog društva, 92, no. 1 (2012):91-104,
https://hdl.handle.net/21.15107/rcub_gery_527 .

TY  - JOUR
AU  - Tadić, Milutin
AU  - Petrović, Aleksandar S.
PY  - 2011
UR  - https://gery.gef.bg.ac.rs/handle/123456789/419
AB  - The subject of the paper is an exact analysis of the orientation of the Serbian monastery churches: the Church of the Virgin Mary (13th century), St. Nicholas' Church (13th century), and an early Christian church (6th century). The paper determines the azimuth of parallel axes in churches, and then the aberrations of those axes from the equinoctial east are interpreted. Under assumption that the axes were directed towards the rising sun, it was surmised that the early Christian church's patron saint could be St. John the Baptist, that the Church of the Virgin Mary was founded on Annunciation day to which it is dedicated, and that St. Nicholas' Church is oriented in accordance with the rule ('toward the sunrise') even though its axis deviates from the equinoctial east by 41° degrees.
AB  - Tema rada jeste egzaktna analiza orijentacije crkava srpskog manastira Gradac: Bogorodičine crkve (13. vek), crkve sv. Nikole (13. vek) i ranohrišćanske crkve (6. vek). U radu su određeni azimuti uzdužnih osa crkava, a zatim su protumačeni otkloni tih osa od ravnodnevačkog istoka. Pod pretpostavkom da su ose usmeravane prema izlazećem suncu, zaključeno je da bi patron ranohrišćanske crkve mogao biti sv. Jovan Krstitelj, da je Bogorodičina crkva zasnovana na praznik Blagovesti kojem je i posvećena, a da je crkva sv. Nikole orijentisana u skladu sa pravilom ('prema izlasku sunca') iako je njena osa otklonjena 41° od ravnodnevačkog istoka.
PB  - Beograd : Srpsko geografsko društvo
T2  - Glasnik Srpskog geografskog društva
T1  - Mathematical-geographical intention in orienting mediaeval churches of the Serbian monastery Gradac
T1  - Matematičko-geografski smisao orijentacije srednjovekovnih crkava srpskog manastira Gradac
VL  - 91
IS  - 4
SP  - 141
EP  - 158
UR  - https://hdl.handle.net/21.15107/rcub_gery_419
ER  - 

@article{
author = "Tadić, Milutin and Petrović, Aleksandar S.",
year = "2011",
abstract = "The subject of the paper is an exact analysis of the orientation of the Serbian monastery churches: the Church of the Virgin Mary (13th century), St. Nicholas' Church (13th century), and an early Christian church (6th century). The paper determines the azimuth of parallel axes in churches, and then the aberrations of those axes from the equinoctial east are interpreted. Under assumption that the axes were directed towards the rising sun, it was surmised that the early Christian church's patron saint could be St. John the Baptist, that the Church of the Virgin Mary was founded on Annunciation day to which it is dedicated, and that St. Nicholas' Church is oriented in accordance with the rule ('toward the sunrise') even though its axis deviates from the equinoctial east by 41° degrees., Tema rada jeste egzaktna analiza orijentacije crkava srpskog manastira Gradac: Bogorodičine crkve (13. vek), crkve sv. Nikole (13. vek) i ranohrišćanske crkve (6. vek). U radu su određeni azimuti uzdužnih osa crkava, a zatim su protumačeni otkloni tih osa od ravnodnevačkog istoka. Pod pretpostavkom da su ose usmeravane prema izlazećem suncu, zaključeno je da bi patron ranohrišćanske crkve mogao biti sv. Jovan Krstitelj, da je Bogorodičina crkva zasnovana na praznik Blagovesti kojem je i posvećena, a da je crkva sv. Nikole orijentisana u skladu sa pravilom ('prema izlasku sunca') iako je njena osa otklonjena 41° od ravnodnevačkog istoka.",
publisher = "Beograd : Srpsko geografsko društvo",
journal = "Glasnik Srpskog geografskog društva",
title = "Mathematical-geographical intention in orienting mediaeval churches of the Serbian monastery Gradac, Matematičko-geografski smisao orijentacije srednjovekovnih crkava srpskog manastira Gradac",
volume = "91",
number = "4",
pages = "141-158",
url = "https://hdl.handle.net/21.15107/rcub_gery_419"
}

Tadić, M.,& Petrović, A. S.. (2011). Mathematical-geographical intention in orienting mediaeval churches of the Serbian monastery Gradac. in Glasnik Srpskog geografskog društva
Beograd : Srpsko geografsko društvo., 91(4), 141-158.
https://hdl.handle.net/21.15107/rcub_gery_419

Tadić M, Petrović AS. Mathematical-geographical intention in orienting mediaeval churches of the Serbian monastery Gradac. in Glasnik Srpskog geografskog društva. 2011;91(4):141-158.
https://hdl.handle.net/21.15107/rcub_gery_419 .

Tadić, Milutin, Petrović, Aleksandar S., "Mathematical-geographical intention in orienting mediaeval churches of the Serbian monastery Gradac" in Glasnik Srpskog geografskog društva, 91, no. 4 (2011):141-158,
https://hdl.handle.net/21.15107/rcub_gery_419 .