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Pregled bibliografske jedinice broj: 512001

Geological maps of Neogene sediments in the Bjelovar Subdepression (northern Croatia)


Malvić, Tomislav
Geological maps of Neogene sediments in the Bjelovar Subdepression (northern Croatia) // Journal of Maps, 2011 (2011), S.I.; 304-317 doi:10.4113/jom.2011.1185 (međunarodna recenzija, članak, znanstveni)


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Naslov
Geological maps of Neogene sediments in the Bjelovar Subdepression (northern Croatia)

Autori
Malvić, Tomislav

Izvornik
Journal of Maps (1744-5647) 2011 (2011), S.I.; 304-317

Vrsta, podvrsta i kategorija rada
Radovi u časopisima, članak, znanstveni

Ključne riječi
subsurface; Neogene; structures; thickness; Croatia

Sažetak
The methods applied in this paper constitute the usual interpolations in subsurface geological mapping that pertain to basin analysis of the Bjelovar Subdepression in northern Croatia. This area covers about 2900 km2, which is the usual scale of small basins within the Pannonian Basin System. The interpolations were constructed along six markers that are stratigraphical and lithostratigraphical borders. These maps provide results for (1) spatial and temporal evolution of sediments and structures, (2) spatial distribution of possible hydrocarbon traps, (3) evaluation of location of mature source rock and (4) fault activity through the Neogene and Quaternary. Large unconformities are present, especially in the eastern portion of the subdepression. There are two main synclines (western and eastern) and several anticlines (Pavljani, Dežanovec...). The fault activity was easily observed, and the slight domination of normal faulting was proven in Badenian– Early Pontian times, and reverse faulting in the Late Pontian– Quaternary. Maximum throws were up to 300 m along some stratigraphical borders.

Izvorni jezik
Engleski

Znanstvena područja
Geologija

Napomena
Rad treba citirati: Malvić, T. (2011) Geological maps of Neogene sediments in the Bjelovar Subdepression (northern Croatia), Journal of Maps, v2011, 304- 317. 10.4113/jom.2011.1185. Kartu treba citirati: Malvić, T. (2011) Published Map. In Malvic, T. (2011) Geological maps of Neogene sediments in the Bjelovar Subdepression (northern Croatia), Journal of Maps, v2011, 304- 317. 10.4113/jom.2011.1185.



POVEZANOST RADA


Projekti:
195-1951293-0237 - Stratigrafska i geomatematička istraživanja naftnogeoloških sustava u Hrvatskoj (Velić, Josipa, MZOS ) ( CroRIS)

Ustanove:
Rudarsko-geološko-naftni fakultet, Zagreb

Profili:

Avatar Url Tomislav Malvić (autor)

Citiraj ovu publikaciju:

Malvić, Tomislav
Geological maps of Neogene sediments in the Bjelovar Subdepression (northern Croatia) // Journal of Maps, 2011 (2011), S.I.; 304-317 doi:10.4113/jom.2011.1185 (međunarodna recenzija, članak, znanstveni)
Malvić, T. (2011) Geological maps of Neogene sediments in the Bjelovar Subdepression (northern Croatia). Journal of Maps, 2011 (S.I.), 304-317 doi:10.4113/jom.2011.1185.
@article{article, author = {Malvi\'{c}, Tomislav}, year = {2011}, pages = {304-317}, DOI = {10.4113/jom.2011.1185}, keywords = {subsurface, Neogene, structures, thickness, Croatia}, journal = {Journal of Maps}, doi = {10.4113/jom.2011.1185}, volume = {2011}, number = {S.I.}, issn = {1744-5647}, title = {Geological maps of Neogene sediments in the Bjelovar Subdepression (northern Croatia)}, keyword = {subsurface, Neogene, structures, thickness, Croatia} }
@article{article, author = {Malvi\'{c}, Tomislav}, year = {2011}, pages = {304-317}, DOI = {10.4113/jom.2011.1185}, keywords = {subsurface, Neogene, structures, thickness, Croatia}, journal = {Journal of Maps}, doi = {10.4113/jom.2011.1185}, volume = {2011}, number = {S.I.}, issn = {1744-5647}, title = {Geological maps of Neogene sediments in the Bjelovar Subdepression (northern Croatia)}, keyword = {subsurface, Neogene, structures, thickness, Croatia} }

Časopis indeksira:


  • Current Contents Connect (CCC)
  • Web of Science Core Collection (WoSCC)
    • Science Citation Index Expanded (SCI-EXP)
    • Social Science Citation Index (SSCI)
    • SCI-EXP, SSCI i/ili A&HCI
  • Scopus


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