Stratigraphic revision of the Quaternary material from the vicinity of Belgrade and the Serbian segment of the Tisza valley analysed by V.D. Laskarev

Gaudenyi, Tivadar; Nenadić, Draženko; Stejić, Petar; Jovanović, Mladjen; Bogićević, Katarina

doi:10.1016/j.quaint.2014.08.041

Cited by 6 publications

(3 citation statements)

References 14 publications

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“…), as evidenced by numerous data (e.g. IvkovIć, 1966;Mar kovIć, 1985;NENadIć et al, 2011;GaudENyI et al, 2015;kNEžEvIć et al, 2018b;ToLjIć et al, 2014).…”

Section: An Overview Of the Geological Backgroundmentioning

confidence: 92%

Depth geological relations of the wider area of Belgrade - based on the wells and geophysical data

Marinović¹,

Rundić

2020

Geol An Balk Poluos

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The subject work covers the Belgrade wider area with a total area of about 2,000 km2. The authors integrated the principal geological and geophysical data provided by surface works and multidisciplinary elements from the fifty-two wells with depths between 33 and 2,733 m. Explicit paleontological findings of specialized analytists with determinations of macro- and microfauna and flora are presented both from Neogene formations and the older basinal floor. In addition to conventional petrological descriptions of rocks, microscopic determinations of intrusive and extrusive magmatites were also cited. From the enclosed basin space, the mineralization of deep aquifers is also correlative positioned. From the geophysical data for wells deeper than 400 m, records of well logging measurements were used, with markers based on which valid stratigraphic delimitations were made. Seismic survey sections were the basis for spatial shaping of Neogene sedimentation and basin floor configuration. For in-depth geological interpretations, published and repository gravimetric and geomagnetic maps of different sizes and years were consulted. The authors focused primarily on factometric indicators without entering into variable and debatable theoretical schematizations, especially orogenically complex of subbasin tectonics, in dissonant relations with the younger disjunctive shaped configuration which is visually shown in the reference cross-sections both vertically and laterally

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“…), as evidenced by numerous data (e.g. IvkovIć, 1966;Mar kovIć, 1985;NENadIć et al, 2011;GaudENyI et al, 2015;kNEžEvIć et al, 2018b;ToLjIć et al, 2014).…”

Section: An Overview Of the Geological Backgroundmentioning

confidence: 92%

Depth geological relations of the wider area of Belgrade - based on the wells and geophysical data

Marinović¹,

Rundić

2020

Geol An Balk Poluos

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“…According to the observation of Krolopp (1977), the Pleistocene flum inalis beds should not be identified at such depth as 21.69 to 27.75 m, and it could be a mistake in HalavAts (1914) paper regarding the description. We cannot accept this statement because sim ilar situations when the Pleistocene Corbicula beds are quite close to the surface have been in the vicinity of Belgrade (see lithological columns of Makiš, Ada Cignalija, Obrenovac, Sajmište, Pančevo) detailed have been discussed in the paper of Gaudenyi et al (2015b).…”

Section: Corrections Of the Stratigraphic Studies Of Krolopp (1977)mentioning

confidence: 97%

“…Some problems appear to have been solved in the past decade regarding Serbian Quaternary stratigraphy. The term "Eopleistocene" as a stratigraphic unit has been rejected and should now be interpreted as a younger part of Lower Pleistocene (Gaudenyi et al, 2014(Gaudenyi et al, , 2015b. Furthermore, "Corbicula flum inalis beds" should be renamed to Pleistocene Corbicula beds because the systematics of Corbicula require revision.…”

Section: Corrections Of the Stratigraphic Studies Of Krolopp (1977)mentioning

confidence: 99%

The revision of Quaternary stratigraphy of the Zrenjanin artesian well borehole profile (Banat, Vojvodina, Serbia)

Gaudenyi

Nenadić

Jovanović

et al. 2022

Geol An Balk Poluos

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The geological analysis of artesian borehole material from Sombor, Subotica, and Zrenjanin, was in the first campaign of detailed stratigraphic studies of Vojvodina in 1892-1895. The results of Quaternary stratigraphy from Zrenjanin were published by HalavAts m ore than a decade later (1914). The significance of the Zrenjanin, Sombor, and Subotica artesian well profiles for more than a century is considered the representative local profiles for the Quaternary stratigraphy of Vojvodina recognized by Serbian (Yugoslavian) and Hungarian geologists. Significant changes were after the taxonomical revision of molluscan material and its stratigraphic context, which was done through the excellent work of Krolopp in the 1970-ies. Unfortunately, the mentioned changes were not applied in the studies during the geological surveying of former Yugoslavia. The developments in Quaternary geology, changes in the Quater nary chronostratigraphic scale, and the results shown by this paper enable the Lower Pleistocene fluvial deposits to be defined as the Pleistocene Corbicula beds, the Viviparus boeckhi Horizon. The Lower Pleistocene at Zrenjanin was documented from 234.54 to 58.36 m depth. The interval between 234.54 and 208.50 m comprises the Upper Paludina - Viviparus vucotinovici zone, while the Viviparus boeckhi Horizons were identified between 135.18 m and 58.36 m. The interval between 58.36 m and 37.75 m is defined as Pleistocene (Lower- and Middle Pleistocene) based on sedimentological and the molluscan record. The interval from 37.75 m to 21.67 m depth was identified as Middle Pleistocene, according to its lithology and the paleontological material. The fluvial sediments? 21.69 m and 7.31 m depths cannot be determined according to the faunistic data; we can only consider them as Pleistocene age. The Holocene sediment and soil horizons ascend to a 2.90 m depth.

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The revision of Quaternary stratigraphy of the Sombor and Subotica artesian well borehole profiles (Bačka, Vojvodina, Serbia)

Gaudenyi

Nenadić

Jovanović

et al. 2018

Quaternary International

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Stratigraphic revision of the Quaternary material from the vicinity of Belgrade and the Serbian segment of the Tisza valley analysed by V.D. Laskarev

Cited by 6 publications

References 14 publications

Depth geological relations of the wider area of Belgrade - based on the wells and geophysical data

Depth geological relations of the wider area of Belgrade - based on the wells and geophysical data

The revision of Quaternary stratigraphy of the Zrenjanin artesian well borehole profile (Banat, Vojvodina, Serbia)

The revision of Quaternary stratigraphy of the Sombor and Subotica artesian well borehole profiles (Bačka, Vojvodina, Serbia)

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