NissirosV1, PascalFrancis, Corpus, bibRecord, 000002

Vertical displacement trends in the Aegean coastal zone (NE Mediterranean) during the Holocene assessed by geo-archaeological data

Identifieur interne : 000002 ( PascalFrancis/Corpus ); précédent : 000001; suivant : 000003

Vertical displacement trends in the Aegean coastal zone (NE Mediterranean) during the Holocene assessed by geo-archaeological data

Auteurs : Kosmas Pavlopoulos ; Vasilios Kapsimalis ; Katerina Theodorakopoulou ; Ioannis P. Panagiotopoulos

Source :

The Holocene : (Sevenoaks) [ 0959-6836 ] ; 2012.

RBID : Francis:13-0250963

Descripteurs français

Pascal (Inist)
- Mésolithique, Antiquité romaine, Méditerranée, Mer Egée, Crète, Grèce, Holocène, Niveau marin, Géoarchéologie, Sédiment, Géomorphologie, Tectonique, Zone côtière, Cyclades.

English descriptors

KwdEn :
- Aegean Sea, Crete, Geoarcheology, Geomorphology, Greece, Holocene, Mediterranean, Mesolithic, Roman antiquity, Sea level, Sediment, Tectonic.

Abstract

Trends in the vertical displacement (i.e. uplift or subsidence) of the Aegean Sea coastal zone have been assessed by comparing observational data with those derived from the predictive glacio-hydro-isostatic model of Lambeck and Purcell (2005) for a period spanning from the Mesolithic to the late Roman times. The data base comprises published studies that use both geomorphological (with associated biological material) and archaeological sea level indicators/markers. Localities demonstrating uplift of high amplitude were detected in front of the Hellenic Arc (Antikythira, Crete, Rhodes, Nisyros) and in the northeast Aegean region (Thrace), whilst areas experiencing tectonic subsidence were mainly observed in the central Aegean region which is characterized by an extensional tectonic domain. However, regional-scale tectonic particularities have caused uplift in parts of the west and east coast of central Aegean. Tectonically 'stable' sites can be found in the Cyclades Plateau, however, this is due to a balance between uplifting and subsiding movements. Sediment compaction and sediment loading may have affected districts with high sedimentation rates such as the Thessaloniki Plain-Thermaikos Gulf (NW Aegean). Finally, tectonic fragmentation of the coastal area in Minor Asia is responsible for localised uplifting and subsiding events.

Notice en format standard (ISO 2709)

Pour connaître la documentation sur le format Inist Standard.

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A09	`01`	`1`	`ENG`	`@1 Multidisciplinary studies in environmental archaeology with particular reference to China`
A11	`01`	`1`		`@1 PAVLOPOULOS (Kosmas)`
A11	`02`	`1`		`@1 KAPSIMALIS (Vasilios)`
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A14	`01`			`@1 Harokopio University, Department of Geography @3 GRC @Z 1 aut. @Z 3 aut.`
A14	`02`			`@1 Hellenic Centre for Marine Research, Institute of Oceanography @3 GRC @Z 2 aut. @Z 4 aut.`
A15	`01`			`@1 Department of Earth Sciences, the University of Hong-Kong @3 HKG @Z 1 aut.`
A15	`02`			`@1 East China Normal University @3 CHN @Z 2 aut.`
A15	`03`			`@1 Lehigh University @3 USA @Z 3 aut.`
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A44				`@0 0000 @1 © 2013 INIST-CNRS. All rights reserved.`
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A69	`01`	`1`	`FRE`	`@1 Études multidisciplinaires en archéologie environnementale avec une référence particulière à la Chine`
C01	`01`		`ENG`	@0 Trends in the vertical displacement (i.e. uplift or subsidence) of the Aegean Sea coastal zone have been assessed by comparing observational data with those derived from the predictive glacio-hydro-isostatic model of Lambeck and Purcell (2005) for a period spanning from the Mesolithic to the late Roman times. The data base comprises published studies that use both geomorphological (with associated biological material) and archaeological sea level indicators/markers. Localities demonstrating uplift of high amplitude were detected in front of the Hellenic Arc (Antikythira, Crete, Rhodes, Nisyros) and in the northeast Aegean region (Thrace), whilst areas experiencing tectonic subsidence were mainly observed in the central Aegean region which is characterized by an extensional tectonic domain. However, regional-scale tectonic particularities have caused uplift in parts of the west and east coast of central Aegean. Tectonically 'stable' sites can be found in the Cyclades Plateau, however, this is due to a balance between uplifting and subsiding movements. Sediment compaction and sediment loading may have affected districts with high sedimentation rates such as the Thessaloniki Plain-Thermaikos Gulf (NW Aegean). Finally, tectonic fragmentation of the coastal area in Minor Asia is responsible for localised uplifting and subsiding events.
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C03	`05`	`H`	`FRE`	`@0 Crète @2 NG @5 07`
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Format Inist (serveur)

NO :	FRANCIS 13-0250963 INIST
FT :	(La tendande d'un déplacement vertical au niveau de la zone côtière de la mer Egée (Nord-Est de la Méditerranée) au cours de l'Holocène, évalué par des données géo-archéologiques)
ET :	Vertical displacement trends in the Aegean coastal zone (NE Mediterranean) during the Holocene assessed by geo-archaeological data
AU :	PAVLOPOULOS (Kosmas); KAPSIMALIS (Vasilios); THEODORAKOPOULOU (Katerina); PANAGIOTOPOULOS (Ioannis P.); ZONG (Yongqiang); CHEN (Zhongyan); YU (Zicheng)
AF :	Harokopio University, Department of Geography/Grèce (1 aut., 3 aut.); Hellenic Centre for Marine Research, Institute of Oceanography/Grèce (2 aut., 4 aut.); Department of Earth Sciences, the University of Hong-Kong/Hong-Kong (1 aut.); East China Normal University/Chine (2 aut.); Lehigh University/Etats-Unis (3 aut.)
DT :	Publication en série; Papier de recherche; Niveau analytique
SO :	The Holocene : (Sevenoaks); ISSN 0959-6836; Royaume-Uni; Da. 2012; Vol. 22; No. 6; Pp. 717-728; Bibl. 2 p.
LA :	Anglais
EA :	Trends in the vertical displacement (i.e. uplift or subsidence) of the Aegean Sea coastal zone have been assessed by comparing observational data with those derived from the predictive glacio-hydro-isostatic model of Lambeck and Purcell (2005) for a period spanning from the Mesolithic to the late Roman times. The data base comprises published studies that use both geomorphological (with associated biological material) and archaeological sea level indicators/markers. Localities demonstrating uplift of high amplitude were detected in front of the Hellenic Arc (Antikythira, Crete, Rhodes, Nisyros) and in the northeast Aegean region (Thrace), whilst areas experiencing tectonic subsidence were mainly observed in the central Aegean region which is characterized by an extensional tectonic domain. However, regional-scale tectonic particularities have caused uplift in parts of the west and east coast of central Aegean. Tectonically 'stable' sites can be found in the Cyclades Plateau, however, this is due to a balance between uplifting and subsiding movements. Sediment compaction and sediment loading may have affected districts with high sedimentation rates such as the Thessaloniki Plain-Thermaikos Gulf (NW Aegean). Finally, tectonic fragmentation of the coastal area in Minor Asia is responsible for localised uplifting and subsiding events.
CC :	52526; 525122A; 525
FD :	Mésolithique; Antiquité romaine; Méditerranée; Mer Egée; Crète; Grèce; Holocène; Niveau marin; Géoarchéologie; Sédiment; Géomorphologie; Tectonique; Zone côtière; Cyclades
FG :	Europe
ED :	Mesolithic; Roman antiquity; Mediterranean; Aegean Sea; Crete; Greece; Holocene; Sea level; Geoarcheology; Sediment; Geomorphology; Tectonic
EG :	Europe
LO :	INIST-25948.354000182522300110
ID :	13-0250963

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Francis:13-0250963

Le document en format XML

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<front><div type="abstract" xml:lang="en">Trends in the vertical displacement (i.e. uplift or subsidence) of the Aegean Sea coastal zone have been assessed by comparing observational data with those derived from the predictive glacio-hydro-isostatic model of Lambeck and Purcell (2005) for a period spanning from the Mesolithic to the late Roman times. The data base comprises published studies that use both geomorphological (with associated biological material) and archaeological sea level indicators/markers. Localities demonstrating uplift of high amplitude were detected in front of the Hellenic Arc (Antikythira, Crete, Rhodes, Nisyros) and in the northeast Aegean region (Thrace), whilst areas experiencing tectonic subsidence were mainly observed in the central Aegean region which is characterized by an extensional tectonic domain. However, regional-scale tectonic particularities have caused uplift in parts of the west and east coast of central Aegean. Tectonically 'stable' sites can be found in the Cyclades Plateau, however, this is due to a balance between uplifting and subsiding movements. Sediment compaction and sediment loading may have affected districts with high sedimentation rates such as the Thessaloniki Plain-Thermaikos Gulf (NW Aegean). Finally, tectonic fragmentation of the coastal area in Minor Asia is responsible for localised uplifting and subsiding events.</div>
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</fC03>
<fC03 i1="04" i2="H" l="FRE"><s0>Mer Egée</s0>
<s2>NG</s2>
<s5>06</s5>
</fC03>
<fC03 i1="04" i2="H" l="ENG"><s0>Aegean Sea</s0>
<s2>NG</s2>
<s5>06</s5>
</fC03>
<fC03 i1="05" i2="H" l="FRE"><s0>Crète</s0>
<s2>NG</s2>
<s5>07</s5>
</fC03>
<fC03 i1="05" i2="H" l="ENG"><s0>Crete</s0>
<s2>NG</s2>
<s5>07</s5>
</fC03>
<fC03 i1="06" i2="H" l="FRE"><s0>Grèce</s0>
<s2>NG</s2>
<s5>08</s5>
</fC03>
<fC03 i1="06" i2="H" l="ENG"><s0>Greece</s0>
<s2>NG</s2>
<s5>08</s5>
</fC03>
<fC03 i1="07" i2="H" l="FRE"><s0>Holocène</s0>
<s2>NI</s2>
<s5>14</s5>
</fC03>
<fC03 i1="07" i2="H" l="ENG"><s0>Holocene</s0>
<s2>NI</s2>
<s5>14</s5>
</fC03>
<fC03 i1="08" i2="H" l="FRE"><s0>Niveau marin</s0>
<s2>563</s2>
<s5>15</s5>
</fC03>
<fC03 i1="08" i2="H" l="ENG"><s0>Sea level</s0>
<s2>563</s2>
<s5>15</s5>
</fC03>
<fC03 i1="09" i2="H" l="FRE"><s0>Géoarchéologie</s0>
<s2>NI</s2>
<s5>16</s5>
</fC03>
<fC03 i1="09" i2="H" l="ENG"><s0>Geoarcheology</s0>
<s2>NI</s2>
<s5>16</s5>
</fC03>
<fC03 i1="10" i2="H" l="FRE"><s0>Sédiment</s0>
<s5>19</s5>
</fC03>
<fC03 i1="10" i2="H" l="ENG"><s0>Sediment</s0>
<s5>19</s5>
</fC03>
<fC03 i1="11" i2="H" l="FRE"><s0>Géomorphologie</s0>
<s5>20</s5>
</fC03>
<fC03 i1="11" i2="H" l="ENG"><s0>Geomorphology</s0>
<s5>20</s5>
</fC03>
<fC03 i1="12" i2="H" l="FRE"><s0>Tectonique</s0>
<s5>27</s5>
</fC03>
<fC03 i1="12" i2="H" l="ENG"><s0>Tectonic</s0>
<s5>27</s5>
</fC03>
<fC03 i1="13" i2="H" l="FRE"><s0>Zone côtière</s0>
<s4>INC</s4>
<s5>31</s5>
</fC03>
<fC03 i1="14" i2="H" l="FRE"><s0>Cyclades</s0>
<s4>INC</s4>
<s5>34</s5>
</fC03>
<fC07 i1="01" i2="H" l="FRE"><s0>Europe</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="01" i2="H" l="ENG"><s0>Europe</s0>
<s2>NG</s2>
</fC07>
<fN21><s1>238</s1>
</fN21>
</pA>
</standard>
<server><NO>FRANCIS 13-0250963 INIST</NO>
<FT>(La tendande d'un déplacement vertical au niveau de la zone côtière de la mer Egée (Nord-Est de la Méditerranée) au cours de l'Holocène, évalué par des données géo-archéologiques)</FT>
<ET>Vertical displacement trends in the Aegean coastal zone (NE Mediterranean) during the Holocene assessed by geo-archaeological data</ET>
<AU>PAVLOPOULOS (Kosmas); KAPSIMALIS (Vasilios); THEODORAKOPOULOU (Katerina); PANAGIOTOPOULOS (Ioannis P.); ZONG (Yongqiang); CHEN (Zhongyan); YU (Zicheng)</AU>
<AF>Harokopio University, Department of Geography/Grèce (1 aut., 3 aut.); Hellenic Centre for Marine Research, Institute of Oceanography/Grèce (2 aut., 4 aut.); Department of Earth Sciences, the University of Hong-Kong/Hong-Kong (1 aut.); East China Normal University/Chine (2 aut.); Lehigh University/Etats-Unis (3 aut.)</AF>
<DT>Publication en série; Papier de recherche; Niveau analytique</DT>
<SO>The Holocene : (Sevenoaks); ISSN 0959-6836; Royaume-Uni; Da. 2012; Vol. 22; No. 6; Pp. 717-728; Bibl. 2 p.</SO>
<LA>Anglais</LA>
<EA>Trends in the vertical displacement (i.e. uplift or subsidence) of the Aegean Sea coastal zone have been assessed by comparing observational data with those derived from the predictive glacio-hydro-isostatic model of Lambeck and Purcell (2005) for a period spanning from the Mesolithic to the late Roman times. The data base comprises published studies that use both geomorphological (with associated biological material) and archaeological sea level indicators/markers. Localities demonstrating uplift of high amplitude were detected in front of the Hellenic Arc (Antikythira, Crete, Rhodes, Nisyros) and in the northeast Aegean region (Thrace), whilst areas experiencing tectonic subsidence were mainly observed in the central Aegean region which is characterized by an extensional tectonic domain. However, regional-scale tectonic particularities have caused uplift in parts of the west and east coast of central Aegean. Tectonically 'stable' sites can be found in the Cyclades Plateau, however, this is due to a balance between uplifting and subsiding movements. Sediment compaction and sediment loading may have affected districts with high sedimentation rates such as the Thessaloniki Plain-Thermaikos Gulf (NW Aegean). Finally, tectonic fragmentation of the coastal area in Minor Asia is responsible for localised uplifting and subsiding events.</EA>
<CC>52526; 525122A; 525</CC>
<FD>Mésolithique; Antiquité romaine; Méditerranée; Mer Egée; Crète; Grèce; Holocène; Niveau marin; Géoarchéologie; Sédiment; Géomorphologie; Tectonique; Zone côtière; Cyclades</FD>
<FG>Europe</FG>
<ED>Mesolithic; Roman antiquity; Mediterranean; Aegean Sea; Crete; Greece; Holocene; Sea level; Geoarcheology; Sediment; Geomorphology; Tectonic</ED>
<EG>Europe</EG>
<LO>INIST-25948.354000182522300110</LO>
<ID>13-0250963</ID>
</server>
</inist>
</record>

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Vertical displacement trends in the Aegean coastal zone (NE Mediterranean) during the Holocene assessed by geo-archaeological data

Vertical displacement trends in the Aegean coastal zone (NE Mediterranean) during the Holocene assessed by geo-archaeological data

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