Zobrazeno 1 - 10
of 25
pro vyhledávání: '"†Boško Lugović"'
Publikováno v:
Geologia Croatica, Vol 68, Iss 1, Pp 25-49 (2015)
Mafic intrusive rocks are subordinately represented fragments of the oceanic crust in the ophiolite mélange exposedat Mts. Kalnik and Ivanščica located in the NW Dinaric-Vardar ophiolite zone. This ophiolite mélange occurs in thenorthern area of
Externí odkaz:
https://doaj.org/article/efb39cdb088344b2a830028185b2fcb0
Publikováno v:
Archives for Technical Sciences / Arhiv za Tehnicke Nauke. 2021, Issue 24, p17-30. 14p.
Publikováno v:
Archives for Technical Sciences / Arhiv za Tehnicke Nauke. 2020, Issue 22, p1-10. 10p.
Publikováno v:
Archives for Technical Sciences. 1:1-10
Postorogenic volcanic rocks of different Tertiary ages are very common in the Sava-Vardar Zone of the Dinarides and in the southeastern part of adjoing Pannonian Basin. South of the Sava-Vardar Zone, in central Bosnia, Tertiary volcanic rocks occur w
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5d49ea00f5d8d3b9188d9f3e45244f5b
https://doi.org/10.7251/afts.2020.1222.001s
https://doi.org/10.7251/afts.2020.1222.001s
Publikováno v:
Geologia Croatica, Vol 61, Iss 1, Pp 19-26 (2008)
At the western seaward coast of the island of Dugi Otok, unusual goethite mineralization occurs as the infilling of a system of thin crevices in the Upper Cretaceous limestones of the Adriatic carbonate platform. Goethite is exceptionally well ordere
Externí odkaz:
https://doaj.org/article/abf3ef6a02624e4ba42d04764ccefde9
Magmatic rocks of post-Late Eocene magmatic formation are widespread in the Sava segment of SavaVardar suture zone and adjoin areas. The rocks formed as a response to transpressional-transtensional tectonic activity preceded by the Cretaceous-Eocene
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::0abcc662050d9e60091147f97566e294
https://www.bib.irb.hr/1254993
https://www.bib.irb.hr/1254993
Publikováno v:
Geologia Croatica
Volume 73
Issue 2
Volume 73
Issue 2
The Dinaridic segment of Neotethys was affected by a widespread shortening and related subduction-accretion-obduction processes that commenced in the middle Jurassic. In the Dinarides, the Krivaja-Konjuh Ophiolite Complex (KKOC) stands as the largest
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::f6a6a23794cd4b2cdfbb0331039ad881
https://hrcak.srce.hr/242166
https://hrcak.srce.hr/242166
Autor:
Filip Gajšak, Duje Smirčić, Hazim Hrvatović, Boško Lugović, Bogdan Jurkovšek, Dunja Aljinović, Tea Kolar-Jurkovšek
Publikováno v:
Rudarsko-geološko-naftni Zbornik, Vol 31, Iss 2, Pp 1-12 (2016)
Middle Triassic volcaniclastic rocks have been recognized at several localities in the vicinity of Bosansko Grahovo, in the southwestern part of Bosnia and Herzegovina in the External Dinarides. Peculiar types of autoclastic rocks were investigated.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::be2c545c569673e40311dd6cb3a2df71
https://doi.org/10.17794/rgn.2016.2.1
https://doi.org/10.17794/rgn.2016.2.1
Autor:
Duje Smirčić, Boško Lugović, Dunja Aljinović, Hazim Hrvatović, Tea Kolar-Jurkovšek, Bogdan Jurkovšek, Filip Gajšak
Publikováno v:
Rudarsko-geološko-naftni zbornik
Volume 31
Issue 2
Volume 31
Issue 2
Middle Triassic volcanic and volcaniclastic rocks have been recognized at several localities near Bosansko Grahovo, in southwestern part of Bosnia and Herzegovina in the External Dinarides. Peculiar types of autoclastic rocks were investigated. These
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od_______951::ddb39519d82eb9913af15feffc33f2b2
https://hrcak.srce.hr/156708
https://hrcak.srce.hr/156708
Publikováno v:
Geoarchaeology. 27:63-87
Archaeological excavations in Dalmatia have yielded a large amount of Hellenistic pottery that has yet to be archaeometrically analyzed. Stylistic analyses suggest that some vessels were imported, but the bulk of the material must have been produced
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::bbef4eea882c8aa04fa4f659d10bba4c
https://doi.org/10.1002/gea.21379
https://doi.org/10.1002/gea.21379