Zobrazeno 1 - 10
of 64
pro vyhledávání: '"Imre Magyar"'
Publikováno v:
Geologia Croatica, Vol 66, Iss 2, Pp 111-118 (2013)
A classic but very rare “Árpád-type” mollusk assemblage, representing the endemic fauna of the Late Miocene–Early Pliocene Lake Pannon, was discovered in Kozármisleny (near Pécs, southern Hungary). The fossils were collected from silt layer
Externí odkaz:
https://doaj.org/article/c34d492e2bd74b26946a15b348ce733b
Publikováno v:
Geologia Croatica, Vol 69, Iss 2 (2016)
Pannonian (Late Miocene) ostracods were investigated from 7 outcrops, exposing deep-water lacustrine sediments along the western margin of the Transylvanian Basin. Sedimentological patterns in the outcrops indicate deposition in sublittoral to profun
Externí odkaz:
https://doaj.org/article/1cf90ccf99654c90be906e11388dd3ee
Publikováno v:
Geologia Croatica, Vol 46, Iss 1, Pp 63-69 (2010)
The combined use of seismic stratigraphy and mollusc biostratigraphy in Late Neogene lacustrine deposits of the Pannonian basin offers three new approaches:First, the comparison of seismic facies and biofacies facilitates to make a distinction betwee
Externí odkaz:
https://doaj.org/article/8e0e04f3021148948f7f424e41c213cf
Autor:
Imre Magyar
Publikováno v:
Földtani Közlöny. 152:157-163
Magyarországon a kronosztratigráfia tudománya az 1980-as és 1990-es évek során szembesült azzal a jelenséggel, hogy klinotémákkal kitöltött medencékben, mint amilyen a Pannon-tó medre is volt, Steno települési törvényei nem, vagy cs
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e154d2c1abe8e8cc221c87ebe353b602
https://doi.org/10.23928/foldt.kozl.2022.152.2.157
https://doi.org/10.23928/foldt.kozl.2022.152.2.157
Publikováno v:
International Journal of Earth Sciences
5 1571 1551 111 M20 М21 In the late Neogene, the Pannonian Basin in Central Europe was filled with sediments when rivers from the Alps and Carpathians shed their sediment load into Lake Pannon. The most powerful source-to-sink system was that of the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::37b5aecfcdb1443517c16d72e58302d6
https://doi.org/10.1007/s00531-022-02188-z
https://doi.org/10.1007/s00531-022-02188-z
Publikováno v:
Földtani Közlöny. 151:267-274
Dinoflagellate-cyst based biostratigraphy is an important tool in the stratigraphical subdivision and correlation of the Neogene Lake Pannon deposits. A total of 66 palynological samples were investigated from the Pannonian (upper Miocene) marl succe
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b8664df2d0840d306fa406e3e0ce0149
https://doi.org/10.23928/foldt.kozl.2021.151.3.267
https://doi.org/10.23928/foldt.kozl.2021.151.3.267
Autor:
Vivien Csoma, Imre Magyar, Andrea Szuromi-Korecz, Krisztina Sebe, Orsolya Sztanó, Krisztina Buczkó, Emőke Tóth
Publikováno v:
Földtani Közlöny. 151:305-326
The large outcrop at Pécs-Danitzpuszta, southern Hungary, exposes a 65-meter-thick succession of calcareous marls, clay marls and calcareous sands that were deposited during the early history of Lake Pannon, a vast, Caspian-type lake in Central Euro
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::26dc3b3d2c0b712aafb009cd432b3bb1
https://doi.org/10.23928/foldt.kozl.2021.151.3.305
https://doi.org/10.23928/foldt.kozl.2021.151.3.305
Autor:
Andrea Szuromi-Korecz, Imre Magyar, Orsolya Sztanó, Vivien Csoma, Dániel Botka, Krisztina Sebe, Emőke Tóth
Publikováno v:
Földtani Közlöny. 151:275-305
The middle Miocene foraminifera and ostracod record of the Central Paratethys usually reflects stable normal marine epositional environments for the Badenian and more patchy, less stable restricted marine environments for the Sarmatian. A 17 m thick
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::da40f8fa221e39f9f37c10e262802d69
https://doi.org/10.23928/foldt.kozl.2021.151.3.275
https://doi.org/10.23928/foldt.kozl.2021.151.3.275
Publikováno v:
Földtani Közlöny. 151:335-361
As the almost 200-year palaeontological research revealed, the geographical distribution of various fossil mollusk faunas in deposits of the late Neogene Lake Pannon displays a regular pattern. The lake basin was filled by lateral accretion of sedime
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5b3603789f0274f932ff69a98843afd8
https://doi.org/10.23928/foldt.kozl.2021.151.4.335
https://doi.org/10.23928/foldt.kozl.2021.151.4.335
In a recent paper by Palcu et al. (2021: Scientific Reports 11, Art. Nr.: 11471), the Cape Panagia section on the Taman peninsula (Russian Black Sea) was dated using magnetostratigraphy, in order to calibrate the timing of previously published regres
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::12a2ced254c76c335dbe35f69f83b700
https://doi.org/10.31223/x5865v
https://doi.org/10.31223/x5865v
