Tectonically controlled Quaternary intracontinental fluvial sequence development in the Nyírség–Pannonian Basin, Hungary

Püspöki, Zoltán; Demeter, Gábor; Tóth-Makk, Ágnes; Kozák, Miklós; Dávid, Árpád; Virág, Magdolna; Kovács-Pálffy, Péter; Kónya, Péter; Gyuricza, Gy.; Kiss, János; McIntosh, Richard William; Forgács, Zoltán; Buday, Tamás; Kovács, Zoltán; Gombos, T.; Kummer, I.

doi:10.1016/j.sedgeo.2012.11.003

Cited by 17 publications

(11 citation statements)

References 41 publications

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“…This is generally made possible in the Quaternary record (e.g., Browne and Naish, 2003;Amorosi et al, 2008;Püspöki et al, 2013.) by a series of favourable conditions including the availability of independently derived proxies for global sea-level history and climatic changes (e.g., Lisiecki and Raymo, 2005;Bertini, 2010).…”

Section: Introductionmentioning

confidence: 99%

Major controls on architecture, sequence stratigraphy and paleosols of middle Pleistocene continental sediments ("Qc Unit"), eastern central Italy

2015

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Middle Pleistocene continental sediments in central Italy ("Qc Unit") record the oldest fluvial accumulation along the uplifting margin of the Peri-Adriatic basin. The architecture of the sediment body can be divided into two unconformity-bounded, fining-upward cycles interpreted as genetically related depositional sequences. These sequences highlight the systematic adjustment of the fluvial systemto changes in the ratio between accommodation space and sediment supply (A/S ratio) and, from base to top, comprise the following surfaces and stratal components: (i) a regionally correlative sequence boundary resulting from an A/S ratio ≤ 0; (ii) a low-accommodation systems tract characterized by conglomerate-rich, amalgamated channel fills and recording an A/S ratio b 1; (iii) an expansion surface marking the turnaround point from low-accommodation systems tract to high-accommodation systems tract deposits; (iv) a high-accommodation systems tract dominated by floodplain fines encasing lens-like, fluvial channel deposits and denoting an A/S ratio N 1; and (v) amature red argillic paleosol. To constrain the climatic signal for paleosols formation, the two sequence-capping mature paleosols have been investigated. The results of these studies suggest that they were developed under humid and warm climatic conditions associated with interglacial phases, which have been correlatively attributed to Marine Oxygen Isotope\ud Stages 11 and 9

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Section: Introductionmentioning

confidence: 99%

Major controls on architecture, sequence stratigraphy and paleosols of middle Pleistocene continental sediments ("Qc Unit"), eastern central Italy

2015

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“…Míg a hordalékkúp peremi részein a folyók még sok kavicsot halmoztak fel, addig a kavicsszintek délnyugat felé fokozatosan kiékelődnek és homokrétegekbe mennek át , Püspöki et al 2013. A hordalékkúpot építő vízfolyások átfolyhattak a területen egészen addig, míg a késő-glaciális során a Tisza át nem váltott a Szatmár-Beregi síkság és a Bodrogköz irányába (Gábris 1998).…”

Section: Bevezetésunclassified

A Maros hordalékkúp fejlődéstörténeti rekonstrukciója

Sümeghy

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“…A composite alluvial fan was built by the Tisza and its tributaries in the foreland of the Northeastern Carpathians in the Pleistocene (Sümeghy 1944;Borsy 1961;Püspöki et al 2013). At the beginning of the Würm (ca 80-70 ka ago) the rivers of the Northeastern Carpathians and Northern Transylvania ran in a north-south or northeast-southwest direction ( Fig.…”

Section: Landscape Evolutionmentioning

confidence: 99%

Landscapes and Landforms of Hungary

Lóczy¹

2015

World Geomorphological Landscapes

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Tectonically controlled Quaternary intracontinental fluvial sequence development in the Nyírség–Pannonian Basin, Hungary

Cited by 17 publications

References 41 publications

Major controls on architecture, sequence stratigraphy and paleosols of middle Pleistocene continental sediments ("Qc Unit"), eastern central Italy

Major controls on architecture, sequence stratigraphy and paleosols of middle Pleistocene continental sediments ("Qc Unit"), eastern central Italy

A Maros hordalékkúp fejlődéstörténeti rekonstrukciója

Landscapes and Landforms of Hungary

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