Results 141 to 150 of about 4,301,896 (195)
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The age of the Sarmatian–Pannonian transition in the Transylvanian Basin (Central Paratethys)
Palaeogeography, Palaeoclimatology, Palaeoecology, 2010A marked paleoenvironmental change took place at the beginning of the late Miocene in the Central Paratethys, with dominantly marine Sarmatian successions grading rapidly into mainly brackish Pannonian deposits. A long and excellently exposed section comprising the Sarmatian-Pannonian transition has been investigated at Oarba de Mure?
Vasiliev, I. +6 more
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Paleoenvironmental evolution of Central Paratethys Sea and Lake Pannon during the Cenozoic
Palaeogeography, Palaeoclimatology, Palaeoecology, 2020Abstract Deep wells penetrated Cenozoic sedimentary record of two different basins: 1) Oligocene retro-arc basin which is buried under the 2) Miocene back-arc Danube Basin. This study is focused on biotic and abiotic proxies discussed in terms of existing biostratigraphical, paleoenvironmental and sedimentological data. Biotic proxies are represented
Tomáš Vlček +10 more
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, 2021
The Menilite facies, representing the most prolific hydrocarbon source rocks in the Carpathian fold and thrust belt, has been studied in two outcrop sections of the Vrancea and Tarcău Nappes (Eastern Romania) with the aim of determining the depositional ...
Małgorzata Wendorff-Belon +2 more
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The Menilite facies, representing the most prolific hydrocarbon source rocks in the Carpathian fold and thrust belt, has been studied in two outcrop sections of the Vrancea and Tarcău Nappes (Eastern Romania) with the aim of determining the depositional ...
Małgorzata Wendorff-Belon +2 more
semanticscholar +1 more source
Fragmenta Palaeontologica Hungarica
Borsodbóta is a well-known Middle Miocene Mollusca site in Hungary, but no Polyplacophora remains have ever been described from there. In recent years, three chiton valves representing three species of three genera (Stenosemus radiatus Dell’Angelo et al.,
Enrico Schwabe, A. Dulai
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Borsodbóta is a well-known Middle Miocene Mollusca site in Hungary, but no Polyplacophora remains have ever been described from there. In recent years, three chiton valves representing three species of three genera (Stenosemus radiatus Dell’Angelo et al.,
Enrico Schwabe, A. Dulai
semanticscholar +1 more source
A review of the Neogene formations and beds in Slovenia, Western Central Paratethys
GeologijaNeogene sedimentary successions are found in eastern and northeastern Slovenia. Their formation was closely related to the evolution of the western part of the Pannonian Basin System and the Central Paratethys; it was influenced by global transgressive ...
Kristina Ivančič +6 more
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Cretaceous evolution of the Central Asian Proto-Paratethys Sea
2020The timing and mechanisms of the Cretaceous sea incursions into Central Asia are still poorly constrained. We provide a new chronostratigraphic framework based on biostratigraphy and magnetostratigraphy together with detailed paleoenvironmental analyses of Cretaceous records of the proto-Paratethys Sea fluctuations in the Tajik and Tarim basins.
Kaya, Mustafa Yuecel (Dr.) +11 more
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Fragmenta Palaeontologica Hungarica
– Várpalota has long been known for its Middle Miocene (mainly mollusc) fossil remains. However, very little information is available on Polyplacophora species. In this paper we discuss the chiton assemblages of two contemporaneous (lower Badenian) sites,
A. Dulai, L. Katona
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– Várpalota has long been known for its Middle Miocene (mainly mollusc) fossil remains. However, very little information is available on Polyplacophora species. In this paper we discuss the chiton assemblages of two contemporaneous (lower Badenian) sites,
A. Dulai, L. Katona
semanticscholar +1 more source
Fragmenta Palaeontologica Hungarica
Seven new Muricidae species are described from the Middle Miocene Central Paratethys from Hungarian and Romanian localities: Murexsul sztanoae n. sp., Attiliosa juhaszi n. sp., Pazinotus martonszaboi n. sp., Gracilipurpura? evae n.
Zoltán Kovács, Z. Vicián
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Seven new Muricidae species are described from the Middle Miocene Central Paratethys from Hungarian and Romanian localities: Murexsul sztanoae n. sp., Attiliosa juhaszi n. sp., Pazinotus martonszaboi n. sp., Gracilipurpura? evae n.
Zoltán Kovács, Z. Vicián
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Miocene Carbonate Platforms in the Polish Carpathians (Central Paratethys). Foraminiferal record
Géologie Méditerranéenne, 1994The Neogene in Central Paratethys was the period when flysch deposition was replaced by that of molasse in both the Carpathian foldbelt and its foredeep. The sedimentation processes were coeval, closely relevant with tectonic phases of the Carpathian orogen evo¬ lution.
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Lower miocene sediments of the Maikop group in the Central Eastern Paratethys
Lithology and Mineral Resources, 2006The composite section of upper Maikop sediments compiled for the central part of the Eastern Paratethys is presented. The section (more than 1000 m) comprises the Karadzhalgan, Sakaraulian, and Kotsakhurian regional stages. The lower boundary of the Miocene drawn at the base of the Karadzhalgan regional stage is unambiguous only in the southern part of
A. S. Stolyarov, E. I. Ivleva
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