Zobrazeno 1 - 10
of 112
pro vyhledávání: '"TIŠLJAR, JOSIP"'
Autor:
VLAHOVIĆ, IGOR, MIKŠA, GORAN, MRINJEK, ERVIN, HASIOTIS, STEPHEN T., VELIĆ, IVO, TIŠLJAR, JOSIP, MATIČEC, DUBRAVKO
Publikováno v:
PALAIOS, 2011 Sep 01. 26(9/10), 567-577.
Externí odkaz:
http://dx.doi.org/10.2110/palo.2011.p11-002r
Evolution of the Adriatic Carbonate Platform: Palaeogeography, main events and depositional dynamics
Publikováno v:
In Palaeogeography, Palaeoclimatology, Palaeoecology 2005 220(3):333-360
Autor:
Matičec, Dubravko, Bergant, Stanislav, Fuček, Ladislav, Palenik, Damir, Korbar, Tvrtko, Vlahović, Igor, Šparica, Marko, Koch, Georg, Prtoljan, Božo, Galović, Ivan, Velić, Ivo, Tišljar, Josip
Ovaj list prikazuje geološku građu, odnosno prostorni raspored, stratigrafske i tektonske odnose te temeljnu paleontologiju i petrologiju 23 litostratigrafskih jedinica različite geološke starosti (jura, kreda, paleogen i kvartar) sjeverozapadnog
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=57a035e5b1ae::aea95cc174d15960bd7c99e5e05f781f
https://www.bib.irb.hr/913281
https://www.bib.irb.hr/913281
Publikováno v:
Geologia Croatica, Vol 50, Iss 1, Pp 17-25 (2010)
Geologia Croatica
Volume 50
Issue 1
Geologia Croatica
Volume 50
Issue 1
The Lower Miocene Macelj-sandstones, from the western part of Hrvatsko Zagorje, are green in colour with variable amounts of glauconitic grains. The Macelj-sandstones were deposited in shallow-marine environments on foreshore, shoreface and tidal fla
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::e23b16e83342d08d0d3ef4eeed9d3299
http://www.geologia-croatica.hr/ojs/index.php/GC/article/view/334
http://www.geologia-croatica.hr/ojs/index.php/GC/article/view/334
Autor:
Matičec, Dubravko, Velić, Ivo, Tišljar, Josip, Vlahović, Igor, Marinčić, Stanko, Fuček, Ladislav
Ovaj list prikazuje geološku građu, odnosno prostorni raspored, stratigrafske i tektonske odnose te temeljnu paleontologiju i petrologiju 13 litostratigrafskih jedinica različite geološke starosti (jura, kreda i kvartar) zapadnog dijela Istre. Li
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=57a035e5b1ae::f59c79c682f33387695ca2e96a6f26bb
https://www.bib.irb.hr/793378
https://www.bib.irb.hr/793378
This paper contains the results of lithofacies and sedimentological interpretations of 6 cores from the Mudawara-1 exploration well drilled in the “ Aphamia block” in Syria. - The oldest part of the deposits: Core-7 (3095.0-3077.4 m) is represent
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=57a035e5b1ae::2101b9ffb120347bb61db0c48a15e722
https://www.bib.irb.hr/284296
https://www.bib.irb.hr/284296
Autor:
Vlahović, Igor, Tišljar, Josip, Velić, Ivo, Matičec, Dubravko, Skelton, Peter, Korbar, Tvrtko, Fuček, Ladislav
During the Kimmeridgian-early Tithonian emersion area of the present Istria represented morphologically diversified terrain affected by significant karstification. On the Zlatni rt cape and Rovinj-1 bauxite deposit near Rovinj there are different typ
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=57a035e5b1ae::0d8d5b44d96557b8f4c8acbf0e3bafb7
https://www.bib.irb.hr/140258
https://www.bib.irb.hr/140258
Istria belongs to the NW part of the ancient Adriatic Carbonate Platform (AdCP), which represented a part of the so-called Mediterannean Seuill (DERCOURT et al., 1993), dividing during the Mesozoic Tethyan realm into the western and eastern part. Due
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=57a035e5b1ae::ddf4b0667e8bc78b917000fdaa58795b
https://www.bib.irb.hr/140231
https://www.bib.irb.hr/140231
The following are examinated regional subaerial unconformities: clayey bauxites associated with Kimmeridgian to Early Tithonian emergence, greenish-gray clays associated with Late Aptian - Late Albian regional emergence, regional scale silicification
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=57a035e5b1ae::960ae1f42508f0f9c4547071c5efc27f
https://www.bib.irb.hr/140404
https://www.bib.irb.hr/140404
Istrian flysch deposits (Istrian Eocene clastics) crop out in the Trieste-Pazin, Labin and Plomin basins, Mt. Učka, and partly on Mt. Ćićarija. They are generally characterized by an alternation of hemipelagic marls and gravity-flow deposits. The
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=57a035e5b1ae::498c3e61a6957c73a1612532e83b1e3a
https://www.bib.irb.hr/140363
https://www.bib.irb.hr/140363