Multiple late-Holocene tsunami landfall in the eastern Gulf of Corinth recorded in the palaeotsunami geo-archive at Lechaion, harbour of ancient Corinth (Peloponnese, Greece)
Identifieur interne : 000098 ( PascalFrancis/Corpus ); précédent : 000097; suivant : 000099Multiple late-Holocene tsunami landfall in the eastern Gulf of Corinth recorded in the palaeotsunami geo-archive at Lechaion, harbour of ancient Corinth (Peloponnese, Greece)
Auteurs : H. Hadler ; A. Vött ; B. Koster ; M. Mathes-Schmidt ; T. Mattern ; K. Ntageretzis ; K. Reicherter ; T. Willersh UserSource :
- Zeitschrift für Geomorphologie [ 0372-8854 ] ; 2013.
Descripteurs français
- Pascal (Inist)
English descriptors
- KwdEn :
Abstract
In this paper, the AA. present geomorphological and geo-scientific evidence of repeated tsunami impact on Lechaion, the harbour of ancient Corinth and adjacent coastal zones of the Gulf of Corinth. Geomorphological, sedimentological, geoarchaeological, geochemical and microfaunal studies as well as geophysical methods revealed evidence of multiple palaeotsunami landfall at the harbour site and surrounding coastal area. Tsunami signatures include coarse-grained, sandy to gravelly allochthonous marine sediments intersecting silt-dominated quiescent harbour deposits, geo-archaeological destruction layers as well as extensive units of beachrock-type calcarenitic tsunamites. A local event-geochronostratigraphy was established by radiocarbon dating and geoarchaeological findings
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Format Inist (serveur)
NO : | FRANCIS 28163890 PRODIG-INTERGEO |
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ET : | Multiple late-Holocene tsunami landfall in the eastern Gulf of Corinth recorded in the palaeotsunami geo-archive at Lechaion, harbour of ancient Corinth (Peloponnese, Greece) |
AU : | HADLER (H.); VÖTT (A.); KOSTER (B.); MATHES-SCHMIDT (M.); MATTERN (T.); NTAGERETZIS (K.); REICHERTER (K.); WILLERSHÄUSER (T.); VÖTT (A.); REICHERTER (K.); PAPANIKOLAOU (I.) |
AF : | Inst. of Geography, Johannes-Gutenberg Univ./Mainz/Allemagne (1 aut., 2 aut., 6 aut., 8 aut.); Neotectonics and Natural Hazards Group, RWTH, Univ./Aachen/Allemagne (3 aut., 4 aut., 7 aut.); Fac. of Classical Archaeology, Univ./Trier/Allemagne (5 aut.); Natural Hazard Research and Geoarcheology, Inst. for Geography, Johannes Gutenberg Univ./Mainz/Allemagne (9 aut.); Inst. of Neotectonics and Natural Hazards, RWTH Univ./Aachen/Allemagne (10 aut.); Lab. of Mineralogy & Geology, Dept. of Geological Sciences and Atmospheric Environment, Agricultural Univ./Athens/Grèce (11 aut.) |
DT : | Publication en série; Niveau analytique |
SO : | Zeitschrift für Geomorphologie; ISSN 0372-8854; Coden ZGMPAG; Allemagne; Da. 2013; Vol. 57; No. 4 Supl.; Pp. 139-180; Bibl. 6 p.; 10 fig., 2 tabl. |
LA : | Anglais |
EA : | In this paper, the AA. present geomorphological and geo-scientific evidence of repeated tsunami impact on Lechaion, the harbour of ancient Corinth and adjacent coastal zones of the Gulf of Corinth. Geomorphological, sedimentological, geoarchaeological, geochemical and microfaunal studies as well as geophysical methods revealed evidence of multiple palaeotsunami landfall at the harbour site and surrounding coastal area. Tsunami signatures include coarse-grained, sandy to gravelly allochthonous marine sediments intersecting silt-dominated quiescent harbour deposits, geo-archaeological destruction layers as well as extensive units of beachrock-type calcarenitic tsunamites. A local event-geochronostratigraphy was established by radiocarbon dating and geoarchaeological findings |
CC : | 531284; 531 |
FD : | Paléogéographie; Littoral; Impact; Tsunami; Chronostratigraphie; Datation C 14; Géoarchéologie; Holocène; Sédimentologie; Grèce; Pelopónnisos; Korinthiakos kolpos |
ED : | Palaeogeography; Coastal environment; Impact; Tsunami; Chronostratigraphy; C 14 dating; Geoarchaeology; Holocene; Sedimentology; Greece; Peloponnese |
SD : | Paleogeografía; Litoral; Impacto; Tsunami; Cronoestratigrafía; Datación Carbono 14; Geoarqueología; Holoceno; Sedimentología; Grecia; Peloponeso |
LO : | INIST-8829 |
ID : | 28163890 |
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Francis:28163890Le document en format XML
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<front><div type="abstract" xml:lang="en">In this paper, the AA. present geomorphological and geo-scientific evidence of repeated tsunami impact on Lechaion, the harbour of ancient Corinth and adjacent coastal zones of the Gulf of Corinth. Geomorphological, sedimentological, geoarchaeological, geochemical and microfaunal studies as well as geophysical methods revealed evidence of multiple palaeotsunami landfall at the harbour site and surrounding coastal area. Tsunami signatures include coarse-grained, sandy to gravelly allochthonous marine sediments intersecting silt-dominated quiescent harbour deposits, geo-archaeological destruction layers as well as extensive units of beachrock-type calcarenitic tsunamites. A local event-geochronostratigraphy was established by radiocarbon dating and geoarchaeological findings</div>
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<fC03 i1="07" i2="G" l="SPA"><s0>Geoarqueología</s0>
<s2>NI</s2>
<s5>07</s5>
</fC03>
<fC03 i1="08" i2="G" l="FRE"><s0>Holocène</s0>
<s2>NI</s2>
<s5>08</s5>
</fC03>
<fC03 i1="08" i2="G" l="ENG"><s0>Holocene</s0>
<s2>NI</s2>
<s5>08</s5>
</fC03>
<fC03 i1="08" i2="G" l="SPA"><s0>Holoceno</s0>
<s2>NI</s2>
<s5>08</s5>
</fC03>
<fC03 i1="09" i2="G" l="FRE"><s0>Sédimentologie</s0>
<s2>NI</s2>
<s5>09</s5>
</fC03>
<fC03 i1="09" i2="G" l="ENG"><s0>Sedimentology</s0>
<s2>NI</s2>
<s5>09</s5>
</fC03>
<fC03 i1="09" i2="G" l="SPA"><s0>Sedimentología</s0>
<s2>NI</s2>
<s5>09</s5>
</fC03>
<fC03 i1="10" i2="G" l="FRE"><s0>Grèce</s0>
<s2>NG</s2>
<s5>10</s5>
</fC03>
<fC03 i1="10" i2="G" l="ENG"><s0>Greece</s0>
<s2>NG</s2>
<s5>10</s5>
</fC03>
<fC03 i1="10" i2="G" l="SPA"><s0>Grecia</s0>
<s2>NG</s2>
<s5>10</s5>
</fC03>
<fC03 i1="11" i2="G" l="FRE"><s0>Pelopónnisos</s0>
<s2>NG</s2>
<s5>11</s5>
</fC03>
<fC03 i1="11" i2="G" l="ENG"><s0>Peloponnese</s0>
<s2>NG</s2>
<s5>11</s5>
</fC03>
<fC03 i1="11" i2="G" l="SPA"><s0>Peloponeso</s0>
<s2>NG</s2>
<s5>11</s5>
</fC03>
<fC03 i1="12" i2="G" l="FRE"><s0>Korinthiakos kolpos</s0>
<s4>INC</s4>
<s5>12</s5>
</fC03>
<fC04 i1="01" i2="G"><s0>U2</s0>
<s1>10!11!12,01,04,07</s1>
</fC04>
<fC04 i1="02" i2="G"><s0>U1</s0>
<s1>01!03,04,05,07!12,11,10</s1>
</fC04>
<fC04 i1="03" i2="G"><s0>U1</s0>
<s1>02!07,05,04,08!12,11,10</s1>
</fC04>
<fC06><s0>FIS</s0>
<s0>TAS</s0>
</fC06>
</pA>
</standard>
<server><NO>FRANCIS 28163890 PRODIG-INTERGEO</NO>
<ET>Multiple late-Holocene tsunami landfall in the eastern Gulf of Corinth recorded in the palaeotsunami geo-archive at Lechaion, harbour of ancient Corinth (Peloponnese, Greece)</ET>
<AU>HADLER (H.); VÖTT (A.); KOSTER (B.); MATHES-SCHMIDT (M.); MATTERN (T.); NTAGERETZIS (K.); REICHERTER (K.); WILLERSHÄUSER (T.); VÖTT (A.); REICHERTER (K.); PAPANIKOLAOU (I.)</AU>
<AF>Inst. of Geography, Johannes-Gutenberg Univ./Mainz/Allemagne (1 aut., 2 aut., 6 aut., 8 aut.); Neotectonics and Natural Hazards Group, RWTH, Univ./Aachen/Allemagne (3 aut., 4 aut., 7 aut.); Fac. of Classical Archaeology, Univ./Trier/Allemagne (5 aut.); Natural Hazard Research and Geoarcheology, Inst. for Geography, Johannes Gutenberg Univ./Mainz/Allemagne (9 aut.); Inst. of Neotectonics and Natural Hazards, RWTH Univ./Aachen/Allemagne (10 aut.); Lab. of Mineralogy & Geology, Dept. of Geological Sciences and Atmospheric Environment, Agricultural Univ./Athens/Grèce (11 aut.)</AF>
<DT>Publication en série; Niveau analytique</DT>
<SO>Zeitschrift für Geomorphologie; ISSN 0372-8854; Coden ZGMPAG; Allemagne; Da. 2013; Vol. 57; No. 4 Supl.; Pp. 139-180; Bibl. 6 p.; 10 fig., 2 tabl.</SO>
<LA>Anglais</LA>
<EA>In this paper, the AA. present geomorphological and geo-scientific evidence of repeated tsunami impact on Lechaion, the harbour of ancient Corinth and adjacent coastal zones of the Gulf of Corinth. Geomorphological, sedimentological, geoarchaeological, geochemical and microfaunal studies as well as geophysical methods revealed evidence of multiple palaeotsunami landfall at the harbour site and surrounding coastal area. Tsunami signatures include coarse-grained, sandy to gravelly allochthonous marine sediments intersecting silt-dominated quiescent harbour deposits, geo-archaeological destruction layers as well as extensive units of beachrock-type calcarenitic tsunamites. A local event-geochronostratigraphy was established by radiocarbon dating and geoarchaeological findings</EA>
<CC>531284; 531</CC>
<FD>Paléogéographie; Littoral; Impact; Tsunami; Chronostratigraphie; Datation C 14; Géoarchéologie; Holocène; Sédimentologie; Grèce; Pelopónnisos; Korinthiakos kolpos</FD>
<ED>Palaeogeography; Coastal environment; Impact; Tsunami; Chronostratigraphy; C 14 dating; Geoarchaeology; Holocene; Sedimentology; Greece; Peloponnese</ED>
<SD>Paleogeografía; Litoral; Impacto; Tsunami; Cronoestratigrafía; Datación Carbono 14; Geoarqueología; Holoceno; Sedimentología; Grecia; Peloponeso</SD>
<LO>INIST-8829</LO>
<ID>28163890</ID>
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