Historical coseismic uplift on Euboea Island, Greece
| Autor: | Maurice Arnold, Paolo Antonio Pirazzoli, S. Papageorgiou, F. Laborel, J. Laborel, Stathis C. Stiros |
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| Přispěvatelé: | Institute of geology and mineral exploration - Athens (IGME), IGME, Centre des Faibles Radioactivités, Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Centre National de la Recherche Scientifique (CNRS), Laboratoire de géographie physique (LGP), Université Paris 1 Panthéon-Sorbonne (UP1)-Centre National de la Recherche Scientifique (CNRS), Laboratoire d'Ecologie du Benthos et de Biologie Végétale Marine, Université de la Méditerranée - Aix-Marseille 2, Aristotle University of Thessaloniki |
| Jazyk: | angličtina |
| Rok vydání: | 1992 |
| Předmět: |
[SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere Subsidence Structural basin Paleontology Geophysics Space and Planetary Science Geochemistry and Petrology Absolute dating Epicenter Earth and Planetary Sciences (miscellaneous) Island arc Quaternary [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment Seismology Holocene Geology ComputingMilieux_MISCELLANEOUS |
| Zdroj: | Earth and Planetary Science Letters Earth and Planetary Science Letters, 1992, 108 (1-3), pp.109-117. ⟨10.1016/0012-821X(92)90063-2⟩ |
| ISSN: | 0012-821X |
| Popis: | In the Aegean region it is usually accepted that uplift is confined to the southern areas, near the outer island arc, whereas subsidence prevails in the inner basin areas. However, we give evidence of elevated notches andLithophaga shells, dated by AMS14C, showing that Holocene coseismic uplift of the order of about a metre occurred in inner Aegean areas too and affected parts of the coasts of north and central Euboea Island between 510 and 380 B.C. and also possibly between 1050 and 900 B.C. |
| Databáze: | OpenAIRE |
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