Zobrazeno 1 - 10
of 75
pro vyhledávání: '"Igor Vlahović"'
Publikováno v:
Geologia Croatica, Vol 70, Iss 1, Pp 11-25 (2017)
The stratigraphic succession in the Čikola Canyon (part of the North Dalmatian Foreland Basin) was studied in detail to describe both the sedimentological characteristics and fossil assemblages of the Lower Eocene deposits during the initial stage o
Externí odkaz:
https://doaj.org/article/cce6d1056e814091b2117ff4925a0017
Publikováno v:
Remote Sensing, Vol 12, Iss 7, p 1157 (2020)
This study, involving remote sensing, seismology, and geology, revealed complex faulting during the mainshock of the Ston–Slano earthquake sequence (5 September, 1996, Mw = 6.0). The observed DInSAR interferogram fringe patterns could not be explai
Externí odkaz:
https://doaj.org/article/39c3bf579fa54dfdab2d77631753f42a
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
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
Publikováno v:
Geologia Croatica, Vol 49, Iss 1, Pp 117-127 (2010)
In the region of the western Istrian anticline, erosional remains of the transgressive Eocene Foraminiferal limestones overly shallow waterdeposits of Early Cretaceous age (Valanginian, Hauterivian andBarremian). This evidence, together with the ocur
Externí odkaz:
https://doaj.org/article/9b9b0cc04cb24a1991566d8a45b68c59
Stratigraphy and Tectonic Relationships Along the Senj - Ogulin Profile (Velika Kapela Mt., Croatia)
Publikováno v:
Geologia Croatica, Vol 50, Iss 2, Pp 261-268 (2010)
Twelve lithostratigraphic units, representing a 5 km thick succession,have been determined from the Senj -Ogulin profile through theVelika Kapela Mt. This 45 km long sequence lies approximately normalto the Dinaric strike. Carbonate deposits ranging
Externí odkaz:
https://doaj.org/article/13960b6d6bc7430eb22103696d8f98d4
Autor:
Ivo Velić, Igor Vlahović
Publikováno v:
Geologia Croatica, Vol 47, Iss 1, Pp 25-43 (2010)
In the Cenomanian shallow-water carbonates of Northwestern Istria five biostratigraphic zones have been established:CEN-1 Ovalveolina maccagnoae and Sellialveolina viallii biozone in the early Lower Cenomanian;CEN-2 O. maccagnoae to Chrysalidina grad
Externí odkaz:
https://doaj.org/article/c9f4635bcd80438cacf794e3b80e895a
Publikováno v:
Geologia Croatica, Vol 63, Iss 1, Pp 117-125 (2010)
Externí odkaz:
https://doaj.org/article/eb2014aa5ef04d15a5156fd079344696
Publikováno v:
Geologia Croatica, Vol 55, Iss 2, Pp 171-183 (2002)
Croatian geological literature during the mid nineteen-eighties andnineties was marked by the appearance of a new geotectonic conceptof the Dinarides proposing that the recent, very complex structuralsetting is a direct consequence of a specific pala
Externí odkaz:
https://doaj.org/article/e074f5088f6b49ffa2597fc6d3906ddb
Publikováno v:
Geologia Croatica, Vol 55, Iss 2, Pp 121-138 (2002)
Synsedimentary tectonics caused significant differentiation of sedimentary environments of the Adriatic Carbonate Platform during the Kimmeridgian. The most important changes have been recorded in W and central Croatia: along the NW part in present d
Externí odkaz:
https://doaj.org/article/c2e70147d05b4a519748094700009bcf