Palaeobathymetry and palaeogeography of the Bakony Eocene Basin in western Hungary

Báldi-Beke, Mária; Báldi, T.

doi:10.1016/0031-0182(91)90013-h

Cited by 14 publications

(1 citation statement)

References 6 publications

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“…The Middle Eocene palaeogeography and the lithological formations of the New gastropod records from the Cenozoic of Hungary 147/3, 265-282., Budapest, 2017 Új adatok a hazai kainozoos gastropodák ismeretéhez Dudar-Jásd and the Balinka Basins (NE Bakony Mts) was treated e.g. by SZŐTS (1956), BÁLDI-BEKE & BÁLDI (1990) and BÁLDI-BEKE (2003). The diverse Lutetian deposits of Dudar and Balinka known from boreholes and coal mines were discussed by KNAUER & KOPEK (1982) and BERNHARDT (1985), res pectively.…”

Section: Geological Settingmentioning

confidence: 99%

New gastropod records from the Cenozoic of Hungary

Vicián¹,

Krock²,

Kovács³

2017

Földt. Közl.

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ÖsszefoglalásTanulmányunk a magyarországi kainozoos tengeri molluszkafauna pontosabb megismeréséhez járul hozzá 2 lutetiai, 2 egri és 22 badeni korú Gastropoda-faj leírásával, melyek többsége hazánkból ismeretlen volt, vagy csupán faunalistákon szerepelt. 21 faj új előfordulás Magyarországon, 22 esetében ez az első ábrázolás a hazai szakirodalomban. Bemutatjuk a fajok rétegtani és ősföldrajzi elterjedését. Közelmúltbeli terepmunkák, valamint a Magyar Természet -tudományi Múzeum gyűjteménye alapján egy új faj, Lautoconus harzhauseri KOVÁCS nov. sp. is leírásra került.Tárgyszavak: Gastropoda, Paratethys, kainozoos, lutetiai, egri, badeni AbstractIn this paper 26 recently collected Cenozoic marine gastropod species from Hungary are briefly described. Two Lutetian (Eocene), two Egerian (Oligocene) and 22 Badenian (Miocene) species are represented; most of them are newlyrecorded, while others are illustrated for the first time as being present in Hungary. The extended stratigraphic and palaeogeographic ranges of the respective species are summarized and a new taxon is introduced: Lautoconus harzhauseri KOVÁCS nov. sp.

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Section: Geological Settingmentioning

confidence: 99%

New gastropod records from the Cenozoic of Hungary

Vicián¹,

Krock²,

Kovács³

2017

Földt. Közl.

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Geology and History of Evolution of the ALCAPA Mega-Unit

Szederkényi¹,

Kovács²,

Haas

et al. 2012

Geology of Hungary

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Gravity-flow dominated sedimentation on the Buda paleoslope (Hungary): Record of Late Eocene continental escape of the Bakony unit

et al. 1992

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Zusammenfassung AbstractThe Upper Eocene sequence of the Buda Hills consists of fluvial and shallow marine conglomerates, sandstones, bioclastic shallow-water limestone, marlstone and pelagic Globigerina marl. The succession illustrates rapid, overall subsidence of the area, from terrestrial environments to bathyal depths. Sedimentation occurred on slopes situated on the flanks of synsedimentary basement antiforms. Vertical growth of antiforms caused progressive tilting of beds, layerparallel extension by boudinage and faulting, and induced redeposition by mass flow. Antiforms are localised in the dextral Buda/3rs shear zone and in the Buda imbricate stack, which accommodated the dextral displacement. The latter is underlain by blind reverse faults probably merging into a detachment tault at shallow depths. These structures were formed by WNW-ESE oriented compression and NNE-SSW directed tension. The morphological expression of the imbricate stack is the SE-facing Buda slope.The Bakony unit, while "escaping" from the Alps, was bordered by a northern sinistral and a southern dextral shear zone. Synsedimentary tectonics in the Buda

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Palaeobathymetry and palaeogeography of the Bakony Eocene Basin in western Hungary

Cited by 14 publications

References 6 publications

New gastropod records from the Cenozoic of Hungary

New gastropod records from the Cenozoic of Hungary

Geology and History of Evolution of the ALCAPA Mega-Unit

Gravity-flow dominated sedimentation on the Buda paleoslope (Hungary): Record of Late Eocene continental escape of the Bakony unit

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