Zobrazeno 1 - 10
of 26
pro vyhledávání: '"Mraz, Vinko"'
Publikováno v:
Radovi Zavoda za znanstvenoistraživački i umjetnički rad u Bjelovaru / Papers of the Institute for Scientific Research and Artistic Work in Bjelovar. (6):127-136
Externí odkaz:
https://www.ceeol.com/search/article-detail?id=776328
Daruvarske toplice nalaze se u dolini rječice Toplice, između zapadnih obronaka Papuka i „Ilovske depresije“. Pojava termalne vode uvjetovana je geološkom građom i i tektonskim odnosima ovog područja. Termalna voda izbija iz trijaskih vapnen
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::8e124e60928c0fd97c0b00a2d3a87e61
https://www.bib.irb.hr/600233
https://www.bib.irb.hr/600233
The investigated area comprises the north western part of Mt. "Ivančica", which is located at north western Croatia. It is composed of rocks ranging in age from Paleozoic to Quaternary. However, from hydrogeological point of view, Triassic carbonate
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=57a035e5b1ae::c38888a6d4479dbf7d3dc7f6bded259a
https://www.bib.irb.hr/617757
https://www.bib.irb.hr/617757
U dolini rijeke Sunje, između naselja Borojevići i Mečenčani, nalazi se izvorište „Pašino vrelo“ na kojem se drenira podzemna voda karbonatnog vodonosnika badenske starosti i kvartarnog aluvijalnog vodonosnika. Osim istoimenog izvora na izv
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=57a035e5b1ae::7d7d44fda9366082fefc1306ee9d076a
https://www.bib.irb.hr/529350
https://www.bib.irb.hr/529350
At the “Pašino vrelo” source, groundwater is exploited by means of wells which tap a carbonate aquifer of Badenian age. The natural quality of groundwater complies with the provisions of the Regulation on health and safety of drinking water. How
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=57a035e5b1ae::8f930b00c2ca4c63bdc237c35f8b5182
https://www.bib.irb.hr/493017
https://www.bib.irb.hr/493017
Groundwater is the dominant source of drinking water in Croatia. The main carbonate aquifers are situated in karstic part of Croatia. Also, some smaller but very valuable carbonate aquifers are situated in Panonian part of Croatia. During the hydroge
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=57a035e5b1ae::acc1cc6d8c0d090ed315116c8115bb0f
https://www.bib.irb.hr/493031
https://www.bib.irb.hr/493031
“ Pašino vrelo” aquifer system is situated in the valley of Sunja stream, in central part of Croatia near state boundary with Bosnia and Herzegovina. It is composed of two aquifers: the carbonate aquifer which is the most important source of dri
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=57a035e5b1ae::be1e5bdd89f70cfa6ff378512616386e
https://www.bib.irb.hr/428927
https://www.bib.irb.hr/428927
Publikováno v:
Rudarsko-geološko-naftni zbornik
Volume 20
Issue 1
Rudarsko-geološko-naftni Zbornik, Vol 20, Iss 1, Pp 13-25 (2008)
Web of Science
Volume 20
Issue 1
Rudarsko-geološko-naftni Zbornik, Vol 20, Iss 1, Pp 13-25 (2008)
Web of Science
Kalničko gorje izgrađuju stijene raspona starosti kreda-holocen, koje je prema hidrogeološkim značajkama moguće razvrstati u tri osnovne hidrogeološke cjeline: (1) područje sjeverno od središnjeg masiva Kalnika, izgrađeno od nepropusnih i sl
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::6f23ea69a63c56308c4ecb37df4744c6
https://hrcak.srce.hr/30476
https://hrcak.srce.hr/30476
The study area is located in north-western part of Croatia. It is quite developed region where agricultural production is the most important economic branch. In that respect, one of the key factors was certainly the abundance of groundwater accumulat
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=57a035e5b1ae::0f27606224e4d049d3e5a77b0224389e
https://www.bib.irb.hr/375376
https://www.bib.irb.hr/375376
Kalničko gorje izgrađuju stijene raspona starosti kreda-holocen, koje je prema hidrogeološkim značajkama moguće razvrstati u tri osnovne hidrogeološke cjeline: (1) područje sjeverno od središnjeg masiva Kalnika, izgrađeno od nepropusnih i sl
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=57a035e5b1ae::b126c8508adf3875e871f47508316b5f
https://www.bib.irb.hr/375367
https://www.bib.irb.hr/375367