Zobrazeno 1 - 10
of 50
pro vyhledávání: '"Zoran Peh"'
Autor:
Nikolina Ilijanić, Erli Kovačević Galović, Nikola Gizdavec, Ivona Ivkić Filipović, Slobodan Miko, Zoran Peh
Publikováno v:
Frontiers in Earth Science, Vol 10 (2023)
Croatian bauxites are long known for their chemical and physical diversity arisen from their characteristic origin and emplacement within the area of the Adriatic–Dinaric carbonate platform (ADCP). They include eight horizons spanning the period be
Externí odkaz:
https://doaj.org/article/fcfa1bceac024ed295393d65056f8fef
Publikováno v:
Land, Vol 12, Iss 4, p 913 (2023)
Physical and chemical weathering, together with biological and biochemical processes, form soil from bedrock and strongly influence the chemical composition of natural waters. Erosive processes, primarily through the agents of running water and wind,
Externí odkaz:
https://doaj.org/article/3af3fa0db0cd4b659a98fb6d4cefdcc1
Autor:
Ozren Hasan, Slobodan Miko, Nikolina Ilijanić, Dea Brunović, Željko Dedić, Martina Šparica Miko, Zoran Peh
Publikováno v:
Geochemical Transactions, Vol 21, Iss 1, Pp 1-22 (2020)
Abstract The study presented in this work emerged as a result of a multiyear regional geochemical survey based on low-density topsoil sampling and the ensuing geochemical atlas of Croatia. This study focuses on the Dinaric part of Croatia to expound
Externí odkaz:
https://doaj.org/article/6456736987494c7db45e56c6211b78da
Autor:
Nikola Gizdavec, Mateo Gašparović, Slobodan Miko, Borna Lužar-Oberiter, Nikolina Ilijanić, Zoran Peh
Publikováno v:
Remote Sensing, Vol 14, Iss 20, p 5169 (2022)
We explored the potential incorporation of Sentinel-2A imagery for rock unit determination in the Croatian karst region dominated by carbonate rocks. The various lithological units are potential sources of both stone aggregates and dimension stone, a
Externí odkaz:
https://doaj.org/article/989f9785c4d44d5a943bc7327bbbbe71
Autor:
Zoran Peh, Erli Kovačević Galović
Publikováno v:
Geologia Croatica, Vol 69, Iss 2 (2016)
Investigation of the origin and emplacement of Istrian Lower Paleogene Bauxites (ILPB) discussed in this work relies on the recent perspectives on development of the collision-induced diachronous discontinuity surface in the Istrian part of the Adria
Externí odkaz:
https://doaj.org/article/7afdddb37f1348c8969afc64d2ad1b67
Publikováno v:
Geologia Croatica, Vol 65, Iss 1, Pp 53-65 (2012)
Two discriminant function models were created in order to distinguish between major- and trace-element geochemical patterns typical of Lower Palaeogene (Palaeocene, Pc) bauxites formed on the portion of the carbonate platform comprising the Karst or
Externí odkaz:
https://doaj.org/article/459c407fdeab436f888b6c08bb5c7c77
Autor:
Zoran Peh
Publikováno v:
Geologia Croatica, Vol 45, Iss 0, Pp 163-172 (2010)
The method of factor analysis (R-mode) is applied as a tool in thesystem approach to the investigation of a selected geomorphologicalregion in the Northwestem Croatia. The factor model derived fromthe analysis is a mathematical representation of the
Externí odkaz:
https://doaj.org/article/a87480fa37f94246b78080903aa40a3a
Publikováno v:
Geologia Croatica, Vol 48, Iss 1, Pp 67-86 (2010)
Estimation of the anthropogenic over natural contribution in the chemical content of soils and sediments is very important but not easy to measure. Normalization based on either aluminium or iron, as reference conservative elements having supposed na
Externí odkaz:
https://doaj.org/article/5abfc61597984df585cdeccfca7d9693
Autor:
Zoran Peh
Publikováno v:
Geologia Croatica, Vol 50, Iss 1, Pp 79-88 (2010)
Frequency distribution curves can be indicative of the dynamicsand evolutionary development of geomorphological systems. Normallydistributed geomorphological data are a reliable indicator of theequilibrium fluctuations prevalent within such systems.
Externí odkaz:
https://doaj.org/article/bd53c28115da4637bf0e91b00a1afdba
Publikováno v:
Geologia Croatica, Vol 51, Iss 1, Pp 47-58 (2010)
Discriminant analysis of Quaternary sediments in the region of Djurdjevac was performed in order to determine the optimum criteria for distinguishing between previously established groups of deposits. Geological properties utilized in the procedure o
Externí odkaz:
https://doaj.org/article/dbdd3d4dd8bc4fcba286b65d0858b890