Zobrazeno 1 - 10
of 14
pro vyhledávání: '"Crmarić, Ranko"'
Autor:
Miko, Slobodan, Crmarić, Ranko, Durn, Tatjana, Bukovec, Dragan, Benac, Čedomir, Hasan, Ozren, Ilijanić, Nikolina, Correggiari, Anamaria, Petričević, Ivan
The European Marine Observation and Data network (EMODnet) is focused on projects assembling marine data, products and metadata into a standardised and harmonised marine data which are interoperable and free of restrictions on use. EMODnet geology (o
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=57a035e5b1ae::9c421f303bd149d567ca144bba71bfcc
https://www.bib.irb.hr/911737
https://www.bib.irb.hr/911737
Autor:
Miko, Slobodan, Ilijanić, Nikolina, Hasan, Ozren, Razum, Ivan, Durn, Tatjana, Brunović, Dea, Papatheodorou, George, Bakrač, Koraljaka, Hajek Tadesse, Valentina, Šparica Miko, Martina, Crmarić, Ranko
The Croatian coastal region is a part of Maritime Dinaric Alps which coincides with the Adriatic Carbonate Platform (AdCP). Some of the coastal karst depressions/basins (Dalmatian coast) developed into larger lakes (Fig.1.). Sediment core records sho
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=57a035e5b1ae::b018ee2d1b2d4bb538e20ec1d5855054
https://www.bib.irb.hr/911731
https://www.bib.irb.hr/911731
Autor:
Miko, Slobodan, Ilijanić, Nikolina, Hasan, Ozren, Razum, Ivan, Durn, Tatjana, Brunović, Dea, Papatheodorou, George, Bakrač, Koraljka, Hajek Tadesse, Valentina, Crmarić, Ranko
The Croatian coastal region is a part of Maritime Dinaric Alps which and coincides with the Adriatic Carbonate Platform (AdCP). The some of the coastal karst depressions developed into larger lakes, although not numerous (
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=57a035e5b1ae::b799b44d3fee8bfbc366073b7213f149
https://www.bib.irb.hr/831068
https://www.bib.irb.hr/831068
U radu su prikazani novi rezultati istraživanja sedimenata i plitkog podmorja na nekoliko lokacija u sjevernom i srednjem dijelu Jadrana. Za istraživanje je korišten geološko-strukturni dubinomjer (Sub Bottom Profiler) kao metoda indirektnog opa
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=57a035e5b1ae::448c005a5756f7f51f7ead43ebea61e2
https://www.bib.irb.hr/488726
https://www.bib.irb.hr/488726
Autor:
Crmarić, Ranko
U okviru ovog rada istraženi su površinski sedimenti i analizirani snimci karakterističnih trasa podmorja dobiveni geološko-strukturnim dubinomjerom, panoramskim dubinomjerom te uporabom višesnopnog dubinomjera dijela jadranskog mora, područja
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=57a035e5b1ae::d8e384e183b0be53dda58a042f37aa4d
https://www.bib.irb.hr/451752
https://www.bib.irb.hr/451752
The Vinodol Channel, as a part of the Kvarner area (northern Adriatic, Croatia), is located between Vinodol coast (NE) and coast of the Krk Island (SW). Coasts of this channel have irregular triangle shape. Very narrow Tihi Channel connects Vinodol C
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=57a035e5b1ae::b168b21abb9999fec10832523ad90fe7
https://www.bib.irb.hr/365371
https://www.bib.irb.hr/365371
Na zahtjev trgovačkog društva GRGUŠA d.o.o. pristupilo se izradi Dopunskog rudarskog projekta osnovom kojeg su obuhvaćene rezerve odobrene 2007. godine. Bitna odstupanja, u odnosu na ranija rješenja i podatke, očituju se u slijedećem: 1. Utvr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=57a035e5b1ae::4be43376d47fc18910e3366d702b3010
https://www.bib.irb.hr/492404
https://www.bib.irb.hr/492404
Oscilacije morske razine prouzročene klimatskim globalnim promjenama bile su vrlo izražene tijekom pleistocena. Holocenski porast morske razine presudno je utjecalo na slijed sedimentacije u podmorju Kvarnera. U doba niže morske razine, tijekom po
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=57a035e5b1ae::3751fc2149a26e4f668685132a24a74a
https://www.bib.irb.hr/266543
https://www.bib.irb.hr/266543
Autor:
Juračić, Mladen, Crmarić, Ranko
Rijeke u čijem porječju ima više fliškog i ostalog nekarbonatnog materijala nose veće količine čestičnog materijala, te je taloženje na njihovim ušćima intenzivnije (Mirna, Raša, Rječina, Cetina i Neretva), dok rijeke u čijem poriječju
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=57a035e5b1ae::33b915d7d676b08ae45593b1aa40093b
https://www.bib.irb.hr/121118
https://www.bib.irb.hr/121118
U priobalnom i kanalskom dijelu Jadranskog mora, geološka građa je složena. Zato se i na malim razmacima nalaze stijene i tla raznolikih geotehničkih svojstava. Na susjednoj obali i otocima mogu se rijetko naći tako ekstremno različiti geotehni
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=57a035e5b1ae::07b7905974b7692e46f275a17019f4db
https://www.bib.irb.hr/98611
https://www.bib.irb.hr/98611