Zobrazeno 1 - 10
of 89
pro vyhledávání: '"IVO VELIĆ"'
Autor:
JASENKA SREMAC, JOSIPA VELIĆ, MARIJA BOŠNJAK, IVO VELIĆ, KORALJKA BAKRAČ, ANA ŠIMIČEVIĆ, TOMISLAV MALVIĆ, DANIEL FOTOVIĆ
Publikováno v:
Rivista Italiana di Paleontologia e Stratigrafia, Vol 130, Iss 3 (2024)
Polymictic gravels exploited in the vicinity of Rugvica, SE from Zagreb, comprise clasts of various lithology, colour, shape, and size. Pebbles are composed of sedimentary, volcanic and, sporadically, metamorphic rocks. During the field work we recog
Externí odkaz:
https://doaj.org/article/63ab32c48b6c4199822c35b40ed81f8b
Autor:
Ivo Velić, Josipa Velić
Publikováno v:
Rudarsko-geološko-naftni Zbornik, Vol 35, Iss 3, Pp 45-54 (2020)
Majstorska Cesta is a historical road along Velebit Mt., NW of Sveti Rok, preserved in its original state since opening in 1832 and therefore added to the cultural heritage list of the Republic of Croatia in 2007. The road passes through sedimentary
Externí odkaz:
https://doaj.org/article/07fa99897c1d4cf0b47e0668e4c80d19
Publikováno v:
Rudarsko-geološko-naftni Zbornik, Vol 33, Iss 4, Pp 1-12 (2018)
A carbonate cobble was collected in a creek near Slovenj Gradec (Slovenia). It comprises Trochactaeon gastropods as well as foraminifera Fleuryana adriatica and Cuneolina ketini from a subtidal environment with agglutinated and porcelaneous benthic f
Externí odkaz:
https://doaj.org/article/d8c75bc09d394f508905f812ba706d57
Publikováno v:
Rudarsko-geološko-naftni Zbornik, Vol 32, Iss 4, Pp 77-96 (2017)
Numerous accumulation and erosional forms originating from the activity of small valley glaciers or cirque glaciers occur in the highest mountains in Croatia: Velebit (1757 m) and Biokovo (1762 m). They were produced during the Upper Pleistocene, in
Externí odkaz:
https://doaj.org/article/81f464ba364e4d89a6c49b235e6f6d95
Autor:
Jasenka Sremac, Josipa Velić, Marija Bošnjak, Ivo Velić, Davor Kudrnovski, Tamara Troskot-Čorbić
Publikováno v:
Geosciences, Vol 8, Iss 12, p 456 (2018)
Upper Cretaceous deposits in Medvednica Mt. are composed of coarse-grained conglomerates, sandstones, shales and the pelagic Scaglia Limestones. Such deposits in the wider region possess reservoir potential, not previously studied in Northern Croatia
Externí odkaz:
https://doaj.org/article/ab3adec26954458e92e6caa98b31151e
Publikováno v:
Geologia Croatica, Vol 66, Iss 1, Pp 15-28 (2013)
The new larger benthic foraminifer Robustoconus tisljari n. gen., n. sp. is described from Middle Jurassic (Early Bajocian) high-energy shallow-water limestones of the Dubrovnik area in the south-eastern part of the Adriatic Carbonate Platform. Robus
Externí odkaz:
https://doaj.org/article/1d18a5543de14d3ebedc2e049c5587d4
Publikováno v:
Geologia Croatica, Vol 65, Iss 2, Pp 161-206 (2012)
A rich algal assemblage at the Kozica locality, in the northern foothills of Mt. Biokovo, contains, among other forms, Praturlonella salernitana BARATTOLO. In addition, the descriptions of Clypeina bucuri BARATTOLO & ROMANO and C. lucana BARATTOLO &
Externí odkaz:
https://doaj.org/article/c8e7921f3c79419ca2cd1ae20d26f71c
New and poorly known Middle Jurassic larger benthic foraminifera from the Karst Dinarides of Croatia
Autor:
Felix Schlagintweit, Ivo Velić
Publikováno v:
Geologia Croatica, Vol 64, Iss 2, Pp 81-100 (2011)
Some new and poorly known larger benthic foraminifera are described from Middle Jurassic (Upper Aalenian-Bajocian) shallow-water limestones of the Croatian Karst Dinarides. Cymbriaella lorigae FUGAGNOLI is reported for the first time beside its type-
Externí odkaz:
https://doaj.org/article/1361b9357d2d44dca75338e51cdbdc56
Publikováno v:
Geologia Croatica, Vol 64, Iss 1, Pp 1-16 (2011)
A small glacier of cirque-valley type existed during the Late Pleistocene Würm Glacial in the Tudorevo and Mirovo karst valleys of Northern Velebit. Its source was in Tudorevo, and it moved through Dundović Mirovo and Bilensko Mirovo to Baričević
Externí odkaz:
https://doaj.org/article/938cbb101e87479ebc2f5dea6912438a
Publikováno v:
Geologia Croatica, Vol 62, Iss 1, Pp 45-61 (2011)
Post-Carboniferous deposits of the Karst Dinarides were analysed in terms of their palaeomagnetic and rock magnetic properties in order to identify the best sections for comprehensive palaeomagnetic studies on geodynamic and palaeogeographic evolutio
Externí odkaz:
https://doaj.org/article/33393159fb2146058e95c1a72b5a07b8