Zobrazeno 1 - 10
of 26
pro vyhledávání: '"Boško, Lugović"'
Autor:
Duje Smirčić, Boško Lugović, Dunja Aljinović, Hazim Hrvatović, Tea Kolar-Jurkovšek, Bogdan Jurkovšek, Filip Gajšak
Publikováno v:
Rudarsko-geološko-naftni Zbornik, Vol 31, Iss 2, Pp 1-12 (2016)
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://doaj.org/article/0a3758bcb3eb4548ac727a69fd785e21
Publikováno v:
Archives for Technical Sciences / Arhiv za Tehnicke Nauke. 2021, Issue 24, p17-30. 14p.
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. 2020, Issue 22, p1-10. 10p.
Publikováno v:
Rudarsko-geološko-naftni Zbornik, Vol 25, Iss 1, Pp 33-46 (2012)
The samples of partly or completely altered basaltic extrusive rocks from Mt. Medvednica ophiolite mélange were analysed by the optical microscopy and by X-ray powder diffraction (XRD). The chemical composition of minerals from different paragenetic
Externí odkaz:
https://doaj.org/article/bc27e77c8fa241799289d27d5e9c8fc5
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
Autor:
Damir Slovenec, Boško Lugović
Publikováno v:
Geologia Croatica, Vol 65, Iss 3, Pp 435-446 (2012)
Eastern Tethyan Repno oceanic domain (ROD) from Zagorje-Mid-Transdanubian Shear Zone bounds Meliata-Maliak and Dinaric-Vardar oceanic systems. The domain lacks ophiolite complexes and oceanic rocks are restricted into Early Callovian to Late Valangin
Externí odkaz:
https://doaj.org/article/f7e269374bbe4d298623498140c59782
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