Zobrazeno 1 - 6
of 6
pro vyhledávání: '"Bertrand Keraudren"'
Publikováno v:
Géomorphologie relief processus environnement. 6:21-24
Morphologic and stratigraphie remnants of the two latest transgressions ofisotopic stage 5 (5.3 et 5.1) are preserved on the cliff of Malia. They allow the dating of a contrasted tectonic activity during isotop stage 5.1 : first, stepped corrosion be
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::8268ec97ce62697faad4ed3513f734aa
https://doi.org/10.3406/morfo.2000.1040
https://doi.org/10.3406/morfo.2000.1040
Autor:
Vincent Caron, Bertrand Keraudren, Paul Bernier, Rémi Dalongeville, Josette Renault-Miskovsky
Publikováno v:
Géomorphologie relief processus environnement. 6:177-190
Coastal regions in north-eastern Crete offer numerous outcrops of Tyrrhenian formations. Their study reveals sediments corresponding to three main high sea stands during the last interglacial with intercalations of aeolianite. The three transgression
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::46d250ba5dc09dfa5e1cd6ef12c3eebd
https://doi.org/10.3406/morfo.2000.1061
https://doi.org/10.3406/morfo.2000.1061
Publikováno v:
Quaternary Science Reviews. 14:605-608
Several calcarenite samples from Mezapos area (South Peloponnesus, Greece) have been studied biochemically by extracting the sterols trapped during the sedimentation. The results have shown that specific compounds deposited in Pliocene sediments can
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6828c75c1485136dcee159101c095293
https://doi.org/10.1016/0277-3791(95)00019-l
https://doi.org/10.1016/0277-3791(95)00019-l
Autor:
Denis Sorel, Bertrand Keraudren
Publikováno v:
Marine Geology. 77:99-107
Between Corinth and Xylokastro 20 marine terraces reflect the interaction of the northern Peloponnese uplift and the global eustatic sea-level fluctuations during the last 500,000 years. Correlation of the terraces with oxygen-isotope records in deep
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::87532af7321928f0443f94023087dc88
https://doi.org/10.1016/0025-3227(87)90085-5
https://doi.org/10.1016/0025-3227(87)90085-5
Autor:
Bertrand Keraudren, Claude Thibault
Publikováno v:
Paléorient. 1:141-149
Whereas the oldest formations of the plio-pleistocene marine area can be found in the Caspian South, the Bakinian is only known by boring. An attempt of a further chronology must especially be made on continental sediments : loess and slope colluvium
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::926826d92576dfd8da3aa9ad854ad66f
https://doi.org/10.3406/paleo.1973.4162
https://doi.org/10.3406/paleo.1973.4162
Publikováno v:
Geobios. 13:145-146
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ba3913cb9984be9b34be7c18947db52d
https://doi.org/10.1016/s0016-6995(80)80024-6
https://doi.org/10.1016/s0016-6995(80)80024-6