Results 171 to 180 of about 1,963 (201)
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Basin analysis of the Burdigalian and Early Langhian successions, Kirkuk Basin, Iraq
Geological Society, London, Special Publications, 2007Abstract Two depositional basins were present in the Kirkuk Basin of northeastern Iraq during the Burdigalian and Early Langhian ages (Late Lower–Early Middle Miocene) and have been studied at several oilfields. Both basins display shallowing upward sequences composed of carbonate and evaporite sediments.
A. I. Al-Juboury +2 more
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Burdigalian–Serravalian calcareous nannoplanktons from Qom Formation, North-Center Iran
Arabian Journal of Geosciences, 2009The aim of this study is to determine calcareous nannofossil species found in Kamar-Kuh area and demonstrate this use for biostratigraphic studies. The Qom Formation is widely distributed in Kamar-Kuh section and has nine members(a–f). In this study, 12 samples were taken and prepared with smear slide.
Hadavi Fatemeh
exaly +2 more sources
78th EAGE Conference and Exhibition 2016, 2016
Sands of the Lower Miocene Traisen Formation in the Lower Austrian Molasse Basin represent a clastic interval correlated with the global sea level drop Bur3 (Burdigalian). Drill cores from OMV-wells in deep parts in the NE show hundreds of meters of pelites with intersections of sands. Profiles of carbonate content, XRD, XRF, whole rock chemistry, clay
Palzer-Khomenko, M. +5 more
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Sands of the Lower Miocene Traisen Formation in the Lower Austrian Molasse Basin represent a clastic interval correlated with the global sea level drop Bur3 (Burdigalian). Drill cores from OMV-wells in deep parts in the NE show hundreds of meters of pelites with intersections of sands. Profiles of carbonate content, XRD, XRF, whole rock chemistry, clay
Palzer-Khomenko, M. +5 more
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Chapter A3 The burdigalian historical stratotype in the rhodanian area
1995Publisher Summary This chapter discusses the Burdigalian historical stratotype in the Rhodanian area. In the stratotype, on top of the upper Cretaceous channelized white sands (Pied Cros quarry) the basal conglomerate with perforated greenish clasts marking the beginning of the Burdigalian transgression is easily visible. In Montbrison-Fontbonau, the
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Rendiconti Online della Società Geologica Italiana, 2011
A stratigraphic and sedimentological analysis of the Miocene spongolitic unit from Central Apennines is presented. The spongolitic succession of the Latium-Abruzzi Platform (informally named Guadagnolo Formation) represents the sedimentation along the platform margin domain.
BRANDANO, Marco, CORDA, Laura
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A stratigraphic and sedimentological analysis of the Miocene spongolitic unit from Central Apennines is presented. The spongolitic succession of the Latium-Abruzzi Platform (informally named Guadagnolo Formation) represents the sedimentation along the platform margin domain.
BRANDANO, Marco, CORDA, Laura
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Diversity of the Early-Miocene Burdigalian) Ostracoda from Northeastern Semnan, Central Iran
2022Seven genera and seventeen species of marine Ostracoda are reported for the first time from the Attari section (Qom Formation), northeast of the Semnan, Central Iran. In this section, the Qom Formation outcrops with 280 m thickness lies on the Eocene volcanic and under the Upper Red formation.
Chegini, Alireza +2 more
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Micropaleontology, 1990
The earliest Miocene strata on the Middle Atlantic Coastal Plain were deposited in two distinct marine transgressions separated by a hiatus in sedimentation of approximately one million years. The older unit (Bed 3A of the Calvert Formation and its correlatives) was deposited in a relatively restricted basin of middle Burdigalian (middle early Miocene)
Karen L. Wetmore, George W. Andrews
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The earliest Miocene strata on the Middle Atlantic Coastal Plain were deposited in two distinct marine transgressions separated by a hiatus in sedimentation of approximately one million years. The older unit (Bed 3A of the Calvert Formation and its correlatives) was deposited in a relatively restricted basin of middle Burdigalian (middle early Miocene)
Karen L. Wetmore, George W. Andrews
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Coral bioconstruction variability in a small basin: the Burdigalian Bonifacio basin (South Corsica).
2014Coral-rich deposits and coral bioconstructions characterize the mixed carbonate-siliciclastic systems developed in the Bonifacio Basin during the Early Miocene. Accurate mapping on photomosaics allowed to document the internal organization of coral deposits as well as lateral and vertical facies relationships.
MAZZUCCHI, ANDREA +3 more
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2009
Bu çalışmada Polypodiaceae, Osmundaceae, Ulmus, Pinus haploxylon–tip , Picea–Pinaceae, Cupressaceae, Castaneae, Cyrillaceae, Oleaceae, Poaceae, Carya, Engelhardia, Quercus, Taxodiaceae, Salix ve Myricaceae formları ile temsil edilen ve Neojen memeli zonlarından MN 5-6 sınırına karşılık gelen Burdigaliyen-Langiyen palinoflorası Muğla-Milas-Ören Kultak ...
KAYSERİ, Mine Sezgül, AKGÜN, Funda
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Bu çalışmada Polypodiaceae, Osmundaceae, Ulmus, Pinus haploxylon–tip , Picea–Pinaceae, Cupressaceae, Castaneae, Cyrillaceae, Oleaceae, Poaceae, Carya, Engelhardia, Quercus, Taxodiaceae, Salix ve Myricaceae formları ile temsil edilen ve Neojen memeli zonlarından MN 5-6 sınırına karşılık gelen Burdigaliyen-Langiyen palinoflorası Muğla-Milas-Ören Kultak ...
KAYSERİ, Mine Sezgül, AKGÜN, Funda
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2015
There is still a considerable controversy about the Oligocene-Miocene chronostratigraphic correlation within the Paratethys domain. Especially in the German and Swiss Molasse basins a robust correlation framework is missing for the late Early Miocene, represented by the lithostratigraphic units of the Upper Marine Molasse (OMM), Upper Brackish Molasse (
Kirscher, U. +6 more
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There is still a considerable controversy about the Oligocene-Miocene chronostratigraphic correlation within the Paratethys domain. Especially in the German and Swiss Molasse basins a robust correlation framework is missing for the late Early Miocene, represented by the lithostratigraphic units of the Upper Marine Molasse (OMM), Upper Brackish Molasse (
Kirscher, U. +6 more
openaire +1 more source

