UnivTrevesV1, PascalFrancis, Corpus, bibRecord, 000098

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 : 000099

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)

Auteurs : H. Hadler ; A. Vött ; B. Koster ; M. Mathes-Schmidt ; T. Mattern ; K. Ntageretzis ; K. Reicherter ; T. Willersh User

Source :

Zeitschrift für Geomorphologie [ 0372-8854 ] ; 2013.

RBID : Francis:28163890

Descripteurs français

Pascal (Inist)
- Paléogéographie, Littoral, Impact, Tsunami, Chronostratigraphie, Datation C 14, Géoarchéologie, Holocène, Sédimentologie, Grèce, Pelopónnisos, Korinthiakos kolpos.

English descriptors

KwdEn :
- C 14 dating, Chronostratigraphy, Coastal environment, Geoarchaeology, Greece, Holocene, Impact, Palaeogeography, Peloponnese, Sedimentology, Tsunami.

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

Notice en format standard (ISO 2709)

Pour connaître la documentation sur le format Inist Standard.

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Format Inist (serveur)

NO :	FRANCIS 28163890 PRODIG-INTERGEO
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

Links to Exploration step

Francis:28163890

Le 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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<fA12 i1="01" i2="1"><s1>VÖTT (A.)</s1>
<s9>dir. publ.</s9>
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<fA12 i1="02" i2="1"><s1>REICHERTER (K.)</s1>
<s9>dir. publ.</s9>
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<fA12 i1="03" i2="1"><s1>PAPANIKOLAOU (I.)</s1>
<s9>dir. publ.</s9>
</fA12>
<fA14 i1="01"><s1>Inst. of Geography, Johannes-Gutenberg Univ.</s1>
<s2>Mainz</s2>
<s3>DEU</s3>
<sZ>1 aut.</sZ>
<sZ>2 aut.</sZ>
<sZ>6 aut.</sZ>
<sZ>8 aut.</sZ>
</fA14>
<fA14 i1="02"><s1>Neotectonics and Natural Hazards Group, RWTH, Univ.</s1>
<s2>Aachen</s2>
<s3>DEU</s3>
<sZ>3 aut.</sZ>
<sZ>4 aut.</sZ>
<sZ>7 aut.</sZ>
</fA14>
<fA14 i1="03"><s1>Fac. of Classical Archaeology, Univ.</s1>
<s2>Trier</s2>
<s3>DEU</s3>
<sZ>5 aut.</sZ>
</fA14>
<fA15 i1="01"><s1>Natural Hazard Research and Geoarcheology, Inst. for Geography, Johannes Gutenberg Univ.</s1>
<s2>Mainz</s2>
<s3>DEU</s3>
<sZ>9 aut.</sZ>
</fA15>
<fA15 i1="02"><s1>Inst. of Neotectonics and Natural Hazards, RWTH Univ.</s1>
<s2>Aachen</s2>
<s3>DEU</s3>
<sZ>10 aut.</sZ>
</fA15>
<fA15 i1="03"><s1>Lab. of Mineralogy & Geology, Dept. of Geological Sciences and Atmospheric Environment, Agricultural Univ.</s1>
<s2>Athens</s2>
<s3>GRC</s3>
<sZ>11 aut.</sZ>
</fA15>
<fA20><s1>139-180</s1>
<s3>10 fig., 2 tabl.</s3>
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</fA21>
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<fA66 i1="01"><s0>DEU</s0>
</fA66>
<fC01 i1="01" l="ENG"><s0>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</s0>
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<s5>01</s5>
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<s5>01</s5>
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<s5>01</s5>
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<s5>02</s5>
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<s2>NI</s2>
<s5>02</s5>
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<fC03 i1="03" i2="G" l="FRE"><s0>Impact</s0>
<s2>NI</s2>
<s5>03</s5>
</fC03>
<fC03 i1="03" i2="G" l="ENG"><s0>Impact</s0>
<s2>NI</s2>
<s5>03</s5>
</fC03>
<fC03 i1="03" i2="G" l="SPA"><s0>Impacto</s0>
<s2>NI</s2>
<s5>03</s5>
</fC03>
<fC03 i1="04" i2="G" l="FRE"><s0>Tsunami</s0>
<s2>NI</s2>
<s5>04</s5>
</fC03>
<fC03 i1="04" i2="G" l="ENG"><s0>Tsunami</s0>
<s2>NI</s2>
<s5>04</s5>
</fC03>
<fC03 i1="04" i2="G" l="SPA"><s0>Tsunami</s0>
<s2>NI</s2>
<s5>04</s5>
</fC03>
<fC03 i1="05" i2="G" l="FRE"><s0>Chronostratigraphie</s0>
<s2>NI</s2>
<s5>05</s5>
</fC03>
<fC03 i1="05" i2="G" l="ENG"><s0>Chronostratigraphy</s0>
<s2>NI</s2>
<s5>05</s5>
</fC03>
<fC03 i1="05" i2="G" l="SPA"><s0>Cronoestratigrafía</s0>
<s2>NI</s2>
<s5>05</s5>
</fC03>
<fC03 i1="06" i2="G" l="FRE"><s0>Datation C 14</s0>
<s2>NI</s2>
<s5>06</s5>
</fC03>
<fC03 i1="06" i2="G" l="ENG"><s0>C 14 dating</s0>
<s2>NI</s2>
<s5>06</s5>
</fC03>
<fC03 i1="06" i2="G" l="SPA"><s0>Datación Carbono 14</s0>
<s2>NI</s2>
<s5>06</s5>
</fC03>
<fC03 i1="07" i2="G" l="FRE"><s0>Géoarchéologie</s0>
<s2>NI</s2>
<s5>07</s5>
</fC03>
<fC03 i1="07" i2="G" l="ENG"><s0>Geoarchaeology</s0>
<s2>NI</s2>
<s5>07</s5>
</fC03>
<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>
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<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>
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<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>
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<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>
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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)

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)

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