Vertical displacement trends in the Aegean coastal zone (NE Mediterranean) during the Holocene assessed by geo-archaeological data
Identifieur interne : 000002 ( PascalFrancis/Checkpoint ); précédent : 000001; suivant : 000003Vertical displacement trends in the Aegean coastal zone (NE Mediterranean) during the Holocene assessed by geo-archaeological data
Auteurs : Kosmas Pavlopoulos [Grèce] ; Vasilios Kapsimalis [Grèce] ; Katerina Theodorakopoulou [Grèce] ; Ioannis P. Panagiotopoulos [Grèce]Source :
- The Holocene : (Sevenoaks) [ 0959-6836 ] ; 2012.
Descripteurs français
- Pascal (Inist)
- Wicri :
- geographic : Grèce.
- topic : Géomorphologie.
English descriptors
- KwdEn :
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.
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Panagiotopoulos</name><affiliation wicri:level="1"><inist:fA14 i1="02"><s1>Hellenic Centre for Marine Research, Institute of Oceanography</s1><s3>GRC</s3><sZ>2 aut.</sZ><sZ>4 aut.</sZ></inist:fA14><country>Grèce</country><wicri:noRegion>Hellenic Centre for Marine Research, Institute of Oceanography</wicri:noRegion></affiliation></author></titleStmt><publicationStmt><idno type="wicri:source">INIST</idno><idno type="inist">13-0250963</idno><date when="2012">2012</date><idno type="stanalyst">FRANCIS 13-0250963 INIST</idno><idno type="RBID">Francis:13-0250963</idno><idno type="wicri:Area/PascalFrancis/Corpus">000002</idno><idno type="wicri:Area/PascalFrancis/Curation">000038</idno><idno type="wicri:Area/PascalFrancis/Checkpoint">000002</idno><idno type="wicri:explorRef" wicri:stream="PascalFrancis" wicri:step="Checkpoint">000002</idno></publicationStmt><sourceDesc><biblStruct><analytic><title xml:lang="en" level="a">Vertical displacement trends in the Aegean coastal zone (NE Mediterranean) during the Holocene assessed by geo-archaeological data</title><author><name sortKey="Pavlopoulos, Kosmas" sort="Pavlopoulos, Kosmas" uniqKey="Pavlopoulos K" first="Kosmas" last="Pavlopoulos">Kosmas Pavlopoulos</name><affiliation wicri:level="4"><inist:fA14 i1="01"><s1>Harokopio University, Department of Geography</s1><s3>GRC</s3><sZ>1 aut.</sZ><sZ>3 aut.</sZ></inist:fA14><country>Grèce</country><wicri:noRegion>Harokopio University, Department of Geography</wicri:noRegion><orgName type="university">Université Harokopio</orgName><placeName><settlement type="city">Athènes</settlement><settlement type="town">Kallithéa</settlement><region nuts="2" type="region">Attique(région)</region></placeName></affiliation></author><author><name sortKey="Kapsimalis, Vasilios" sort="Kapsimalis, Vasilios" uniqKey="Kapsimalis V" first="Vasilios" last="Kapsimalis">Vasilios Kapsimalis</name><affiliation wicri:level="1"><inist:fA14 i1="02"><s1>Hellenic Centre for Marine Research, Institute of Oceanography</s1><s3>GRC</s3><sZ>2 aut.</sZ><sZ>4 aut.</sZ></inist:fA14><country>Grèce</country><wicri:noRegion>Hellenic Centre for Marine Research, Institute of Oceanography</wicri:noRegion></affiliation></author><author><name sortKey="Theodorakopoulou, Katerina" sort="Theodorakopoulou, Katerina" uniqKey="Theodorakopoulou K" first="Katerina" last="Theodorakopoulou">Katerina Theodorakopoulou</name><affiliation wicri:level="4"><inist:fA14 i1="01"><s1>Harokopio University, Department of Geography</s1><s3>GRC</s3><sZ>1 aut.</sZ><sZ>3 aut.</sZ></inist:fA14><country>Grèce</country><wicri:noRegion>Harokopio University, Department of Geography</wicri:noRegion><orgName type="university">Université Harokopio</orgName><placeName><settlement type="city">Athènes</settlement><settlement type="town">Kallithéa</settlement><region nuts="2" type="region">Attique(région)</region></placeName></affiliation></author><author><name sortKey="Panagiotopoulos, Ioannis P" sort="Panagiotopoulos, Ioannis P" uniqKey="Panagiotopoulos I" first="Ioannis P." last="Panagiotopoulos">Ioannis P. Panagiotopoulos</name><affiliation wicri:level="1"><inist:fA14 i1="02"><s1>Hellenic Centre for Marine Research, Institute of Oceanography</s1><s3>GRC</s3><sZ>2 aut.</sZ><sZ>4 aut.</sZ></inist:fA14><country>Grèce</country><wicri:noRegion>Hellenic Centre for Marine Research, Institute of Oceanography</wicri:noRegion></affiliation></author></analytic><series><title level="j" type="main">The Holocene : (Sevenoaks)</title><title level="j" type="abbreviated">Holocene : (Sevenoaks)</title><idno type="ISSN">0959-6836</idno><imprint><date when="2012">2012</date></imprint></series></biblStruct></sourceDesc><seriesStmt><title level="j" type="main">The Holocene : (Sevenoaks)</title><title level="j" type="abbreviated">Holocene : (Sevenoaks)</title><idno type="ISSN">0959-6836</idno></seriesStmt></fileDesc><profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>Aegean Sea</term><term>Crete</term><term>Geoarcheology</term><term>Geomorphology</term><term>Greece</term><term>Holocene</term><term>Mediterranean</term><term>Mesolithic</term><term>Roman antiquity</term><term>Sea level</term><term>Sediment</term><term>Tectonic</term></keywords><keywords scheme="Pascal" xml:lang="fr"><term>Mésolithique</term><term>Antiquité romaine</term><term>Méditerranée</term><term>Mer Egée</term><term>Crète</term><term>Grèce</term><term>Holocène</term><term>Niveau marin</term><term>Géoarchéologie</term><term>Sédiment</term><term>Géomorphologie</term><term>Tectonique</term><term>Zone côtière</term><term>Cyclades</term></keywords><keywords scheme="Wicri" type="geographic" xml:lang="fr"><term>Grèce</term></keywords><keywords scheme="Wicri" type="topic" xml:lang="fr"><term>Géomorphologie</term></keywords></textClass></profileDesc></teiHeader><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></front></TEI><inist><standard h6="B"><pA><fA01 i1="01" i2="1"><s0>0959-6836</s0></fA01><fA03 i2="1"><s0>Holocene : (Sevenoaks)</s0></fA03><fA05><s2>22</s2></fA05><fA06><s2>6</s2></fA06><fA08 i1="01" i2="1" l="ENG"><s1>Vertical displacement trends in the Aegean coastal zone (NE Mediterranean) during the Holocene assessed by geo-archaeological data</s1></fA08><fA09 i1="01" i2="1" l="ENG"><s1>Multidisciplinary studies in environmental archaeology with particular reference to China</s1></fA09><fA11 i1="01" i2="1"><s1>PAVLOPOULOS (Kosmas)</s1></fA11><fA11 i1="02" i2="1"><s1>KAPSIMALIS (Vasilios)</s1></fA11><fA11 i1="03" i2="1"><s1>THEODORAKOPOULOU (Katerina)</s1></fA11><fA11 i1="04" i2="1"><s1>PANAGIOTOPOULOS (Ioannis P.)</s1></fA11><fA12 i1="01" i2="1"><s1>ZONG (Yongqiang)</s1><s9>ed.</s9></fA12><fA12 i1="02" i2="1"><s1>CHEN (Zhongyan)</s1><s9>ed.</s9></fA12><fA12 i1="03" i2="1"><s1>YU (Zicheng)</s1><s9>ed.</s9></fA12><fA14 i1="01"><s1>Harokopio University, Department of Geography</s1><s3>GRC</s3><sZ>1 aut.</sZ><sZ>3 aut.</sZ></fA14><fA14 i1="02"><s1>Hellenic Centre for Marine Research, Institute of Oceanography</s1><s3>GRC</s3><sZ>2 aut.</sZ><sZ>4 aut.</sZ></fA14><fA15 i1="01"><s1>Department of Earth Sciences, the University of Hong-Kong</s1><s3>HKG</s3><sZ>1 aut.</sZ></fA15><fA15 i1="02"><s1>East China Normal University</s1><s3>CHN</s3><sZ>2 aut.</sZ></fA15><fA15 i1="03"><s1>Lehigh University</s1><s3>USA</s3><sZ>3 aut.</sZ></fA15><fA20><s1>717-728</s1></fA20><fA21><s1>2012</s1></fA21><fA23 i1="01"><s0>ENG</s0></fA23><fA43 i1="01"><s1>INIST</s1><s2>25948</s2><s5>354000182522300110</s5></fA43><fA44><s0>0000</s0><s1>© 2013 INIST-CNRS. All rights reserved.</s1></fA44><fA45><s0>2 p.</s0></fA45><fA47 i1="01" i2="1"><s0>13-0250963</s0></fA47><fA60><s1>P</s1><s3>PR</s3></fA60><fA61><s0>A</s0></fA61><fA64 i1="01" i2="1"><s0>The Holocene : (Sevenoaks)</s0></fA64><fA66 i1="01"><s0>GBR</s0></fA66><fA68 i1="01" i2="1" l="FRE"><s1>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</s1></fA68><fA69 i1="01" i2="1" l="FRE"><s1>Études multidisciplinaires en archéologie environnementale avec une référence particulière à la Chine</s1></fA69><fC01 i1="01" l="ENG"><s0>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). 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Panagiotopoulos</name><name sortKey="Theodorakopoulou, Katerina" sort="Theodorakopoulou, Katerina" uniqKey="Theodorakopoulou K" first="Katerina" last="Theodorakopoulou">Katerina Theodorakopoulou</name></country></tree></affiliations></record>Pour manipuler ce document sous Unix (Dilib)
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