NissirosV1, PascalFrancis, Corpus, bibRecord, 000000

Exploring the Avyssos-Yali-Strogyli submarine volcanic complex at the eastern edge of the Aegean Volcanic Arc

Identifieur interne : 000000 ( PascalFrancis/Corpus ); suivant : 000001

Exploring the Avyssos-Yali-Strogyli submarine volcanic complex at the eastern edge of the Aegean Volcanic Arc

Auteurs : P. Nomikou ; K. L. Croff Bell ; D. Papanikolaou ; I. Livanos ; J. Fero Martin

Source :

Zeitschrift für Geomorphologie [ 0372-8854 ] ; 2013.

RBID : Francis:28016309

Descripteurs français

Pascal (Inist)
- Fond sous-marin, Géomorphologie sous-marine, Volcan, Volcanisme, Quaternaire, Bathymétrie, Néotectonique, Fossé tectonique, Stratigraphie, Grèce, Méditerranée, Egée mer.

English descriptors

KwdEn :
- Aegean Sea, Bathymetry, Graben, Greece, Mediterranean Sea, Neotectonics, Quaternary, Sea floor, Stratigraphy, Submarine geomorphology, Volcanism, Volcano.

Abstract

This paper reports the results of the Remotely Operated Vehicle (ROV) exploration combined with multibeam data, providing new information about the main morphological characteristics of the Nisyros submarine volcanic centres. ROV exploration of the eastern flank of Yali revealed wave-type sediment structures, as well as linear fractures at various depths. Several smaller craters were also discovered on the northwest slopes of Strongyli, aligned with ENE-WSW trending fractures with no signs of hydrothermal activity. Heavy biogenic encrustations cover the volcanic rock outcrops on the flanks of both Yali and Strongyli. Analysis of recovered samples will provide information about their relationship to the geology of the nearby islands.

Notice en format standard (ISO 2709)

Pour connaître la documentation sur le format Inist Standard.

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A08	`01`	`1`	`ENG`	`@1 Exploring the Avyssos-Yali-Strogyli submarine volcanic complex at the eastern edge of the Aegean Volcanic Arc`
A09	`01`	`1`	`ENG`	`@1 Quaternary geomorphology in tectonically active areas with emphasis in fluvio-coastal processes`
A11	`01`	`1`		`@1 NOMIKOU (P.)`
A11	`02`	`1`		`@1 CROFF BELL (K.L.)`
A11	`03`	`1`		`@1 PAPANIKOLAOU (D.)`
A11	`04`	`1`		`@1 LIVANOS (I.)`
A11	`05`	`1`		`@1 FERO MARTIN (J.)`
A12	`01`	`1`		`@1 EVELPIDOU (N.) @9 ed.`
A12	`02`	`1`		`@1 PAVLOPOULOS (K.) @9 ed.`
A14	`01`			`@1 Fac. of Geology and Geoenvironment, National and Kapodistrian Univ. @2 Athens @3 GRC @Z 1 aut. @Z 3 aut. @Z 4 aut.`
A14	`02`			`@1 Graduate School of Oceanography, Univ. of Rhode Island @2 Narragansett @3 USA @Z 2 aut. @Z 5 aut.`
A20				`@1 125-137 @3 12 fig.`
A21				`@1 2013`
A23	`01`			`@0 ENG`
A43	`01`			`@1 INIST @2 8829`
A44	`01`			`@0 8200 @1 Tous droits réservés © Prodig - Bibliographie Géographique Internationale (BGI), 2013`
A45				`@0 29 ref.`
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C01	`01`		`ENG`	@0 This paper reports the results of the Remotely Operated Vehicle (ROV) exploration combined with multibeam data, providing new information about the main morphological characteristics of the Nisyros submarine volcanic centres. ROV exploration of the eastern flank of Yali revealed wave-type sediment structures, as well as linear fractures at various depths. Several smaller craters were also discovered on the northwest slopes of Strongyli, aligned with ENE-WSW trending fractures with no signs of hydrothermal activity. Heavy biogenic encrustations cover the volcanic rock outcrops on the flanks of both Yali and Strongyli. Analysis of recovered samples will provide information about their relationship to the geology of the nearby islands.
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C03	`02`	`G`	`ENG`	`@0 Submarine geomorphology @2 NI @5 02`
C03	`02`	`G`	`SPA`	`@0 Geomorfología submarina @2 NI @5 02`
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C03	`03`	`G`	`SPA`	`@0 Volcán @2 NI @5 03`
C03	`04`	`G`	`FRE`	`@0 Volcanisme @2 NI @5 04`
C03	`04`	`G`	`ENG`	`@0 Volcanism @2 NI @5 04`
C03	`04`	`G`	`SPA`	`@0 Volcanismo @2 NI @5 04`
C03	`05`	`G`	`FRE`	`@0 Quaternaire @2 NI @5 05`
C03	`05`	`G`	`ENG`	`@0 Quaternary @2 NI @5 05`
C03	`05`	`G`	`SPA`	`@0 Cuaternario @2 NI @5 05`
C03	`06`	`G`	`FRE`	`@0 Bathymétrie @2 NI @5 06`
C03	`06`	`G`	`ENG`	`@0 Bathymetry @2 NI @5 06`
C03	`06`	`G`	`SPA`	`@0 Batimetría @2 NI @5 06`
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C03	`07`	`G`	`SPA`	`@0 Neotectónica @2 NI @5 07`
C03	`08`	`G`	`FRE`	`@0 Fossé tectonique @2 NI @5 08`
C03	`08`	`G`	`ENG`	`@0 Graben @2 NI @5 08`
C03	`08`	`G`	`SPA`	`@0 Foso tectónico @2 NI @5 08`
C03	`09`	`G`	`FRE`	`@0 Stratigraphie @2 NI @5 09`
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C03	`09`	`G`	`SPA`	`@0 Estratigrafía @2 NI @5 09`
C03	`10`	`G`	`FRE`	`@0 Grèce @2 NG @5 10`
C03	`10`	`G`	`ENG`	`@0 Greece @2 NG @5 10`
C03	`10`	`G`	`SPA`	`@0 Grecia @2 NG @5 10`
C03	`11`	`G`	`FRE`	`@0 Méditerranée @2 NG @5 11`
C03	`11`	`G`	`ENG`	`@0 Mediterranean Sea @2 NG @5 11`
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C04	`01`	`G`		`@0 U2 @1 11!12!02,03,05,07`
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C06				`@0 FIS`

Format Inist (serveur)

NO :	FRANCIS 28016309 PRODIG-INTERGEO
ET :	Exploring the Avyssos-Yali-Strogyli submarine volcanic complex at the eastern edge of the Aegean Volcanic Arc
AU :	NOMIKOU (P.); CROFF BELL (K.L.); PAPANIKOLAOU (D.); LIVANOS (I.); FERO MARTIN (J.); EVELPIDOU (N.); PAVLOPOULOS (K.)
AF :	Fac. of Geology and Geoenvironment, National and Kapodistrian Univ./Athens/Grèce (1 aut., 3 aut., 4 aut.); Graduate School of Oceanography, Univ. of Rhode Island/Narragansett/Etats-Unis (2 aut., 5 aut.)
DT :	Publication en série; Niveau analytique
SO :	Zeitschrift für Geomorphologie; ISSN 0372-8854; Coden ZGMPAG; Allemagne; Da. 2013; Vol. 57; No. 3 Suppl.; Pp. 125-137; Bibl. 29 ref.; 12 fig.
LA :	Anglais
EA :	This paper reports the results of the Remotely Operated Vehicle (ROV) exploration combined with multibeam data, providing new information about the main morphological characteristics of the Nisyros submarine volcanic centres. ROV exploration of the eastern flank of Yali revealed wave-type sediment structures, as well as linear fractures at various depths. Several smaller craters were also discovered on the northwest slopes of Strongyli, aligned with ENE-WSW trending fractures with no signs of hydrothermal activity. Heavy biogenic encrustations cover the volcanic rock outcrops on the flanks of both Yali and Strongyli. Analysis of recovered samples will provide information about their relationship to the geology of the nearby islands.
CC :	53186; 531
FD :	Fond sous-marin; Géomorphologie sous-marine; Volcan; Volcanisme; Quaternaire; Bathymétrie; Néotectonique; Fossé tectonique; Stratigraphie; Grèce; Méditerranée; Egée mer
ED :	Sea floor; Submarine geomorphology; Volcano; Volcanism; Quaternary; Bathymetry; Neotectonics; Graben; Stratigraphy; Greece; Mediterranean Sea; Aegean Sea
SD :	Fondo submarino; Geomorfología submarina; Volcán; Volcanismo; Cuaternario; Batimetría; Neotectónica; Foso tectónico; Estratigrafía; Grecia; El Mediterranéo; Mar Egeo
LO :	INIST-8829
ID :	28016309

Links to Exploration step

Francis:28016309

Le document en format XML

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<front><div type="abstract" xml:lang="en">This paper reports the results of the Remotely Operated Vehicle (ROV) exploration combined with multibeam data, providing new information about the main morphological characteristics of the Nisyros submarine volcanic centres. ROV exploration of the eastern flank of Yali revealed wave-type sediment structures, as well as linear fractures at various depths. Several smaller craters were also discovered on the northwest slopes of Strongyli, aligned with ENE-WSW trending fractures with no signs of hydrothermal activity. Heavy biogenic encrustations cover the volcanic rock outcrops on the flanks of both Yali and Strongyli. Analysis of recovered samples will provide information about their relationship to the geology of the nearby islands.</div>
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<fC01 i1="01" l="ENG"><s0>This paper reports the results of the Remotely Operated Vehicle (ROV) exploration combined with multibeam data, providing new information about the main morphological characteristics of the Nisyros submarine volcanic centres. ROV exploration of the eastern flank of Yali revealed wave-type sediment structures, as well as linear fractures at various depths. Several smaller craters were also discovered on the northwest slopes of Strongyli, aligned with ENE-WSW trending fractures with no signs of hydrothermal activity. Heavy biogenic encrustations cover the volcanic rock outcrops on the flanks of both Yali and Strongyli. Analysis of recovered samples will provide information about their relationship to the geology of the nearby islands.</s0>
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<fC03 i1="05" i2="G" l="SPA"><s0>Cuaternario</s0>
<s2>NI</s2>
<s5>05</s5>
</fC03>
<fC03 i1="06" i2="G" l="FRE"><s0>Bathymétrie</s0>
<s2>NI</s2>
<s5>06</s5>
</fC03>
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<s2>NI</s2>
<s5>06</s5>
</fC03>
<fC03 i1="06" i2="G" l="SPA"><s0>Batimetría</s0>
<s2>NI</s2>
<s5>06</s5>
</fC03>
<fC03 i1="07" i2="G" l="FRE"><s0>Néotectonique</s0>
<s2>NI</s2>
<s5>07</s5>
</fC03>
<fC03 i1="07" i2="G" l="ENG"><s0>Neotectonics</s0>
<s2>NI</s2>
<s5>07</s5>
</fC03>
<fC03 i1="07" i2="G" l="SPA"><s0>Neotectónica</s0>
<s2>NI</s2>
<s5>07</s5>
</fC03>
<fC03 i1="08" i2="G" l="FRE"><s0>Fossé tectonique</s0>
<s2>NI</s2>
<s5>08</s5>
</fC03>
<fC03 i1="08" i2="G" l="ENG"><s0>Graben</s0>
<s2>NI</s2>
<s5>08</s5>
</fC03>
<fC03 i1="08" i2="G" l="SPA"><s0>Foso tectónico</s0>
<s2>NI</s2>
<s5>08</s5>
</fC03>
<fC03 i1="09" i2="G" l="FRE"><s0>Stratigraphie</s0>
<s2>NI</s2>
<s5>09</s5>
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<fC03 i1="09" i2="G" l="ENG"><s0>Stratigraphy</s0>
<s2>NI</s2>
<s5>09</s5>
</fC03>
<fC03 i1="09" i2="G" l="SPA"><s0>Estratigrafía</s0>
<s2>NI</s2>
<s5>09</s5>
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<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>Méditerranée</s0>
<s2>NG</s2>
<s5>11</s5>
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<fC03 i1="11" i2="G" l="ENG"><s0>Mediterranean Sea</s0>
<s2>NG</s2>
<s5>11</s5>
</fC03>
<fC03 i1="11" i2="G" l="SPA"><s0>El Mediterranéo</s0>
<s2>NG</s2>
<s5>11</s5>
</fC03>
<fC03 i1="12" i2="G" l="FRE"><s0>Egée mer</s0>
<s2>NG</s2>
<s5>12</s5>
</fC03>
<fC03 i1="12" i2="G" l="ENG"><s0>Aegean Sea</s0>
<s2>NG</s2>
<s5>12</s5>
</fC03>
<fC03 i1="12" i2="G" l="SPA"><s0>Mar Egeo</s0>
<s2>NG</s2>
<s5>12</s5>
</fC03>
<fC04 i1="01" i2="G"><s0>U2</s0>
<s1>11!12!02,03,05,07</s1>
</fC04>
<fC04 i1="02" i2="G"><s0>U1</s0>
<s1>01!06,02,03,05!12,11</s1>
</fC04>
<fC04 i1="03" i2="G"><s0>U1</s0>
<s1>04!02,05,09,07!12,10</s1>
</fC04>
<fC06><s0>FIS</s0>
</fC06>
</pA>
</standard>
<server><NO>FRANCIS 28016309 PRODIG-INTERGEO</NO>
<ET>Exploring the Avyssos-Yali-Strogyli submarine volcanic complex at the eastern edge of the Aegean Volcanic Arc</ET>
<AU>NOMIKOU (P.); CROFF BELL (K.L.); PAPANIKOLAOU (D.); LIVANOS (I.); FERO MARTIN (J.); EVELPIDOU (N.); PAVLOPOULOS (K.)</AU>
<AF>Fac. of Geology and Geoenvironment, National and Kapodistrian Univ./Athens/Grèce (1 aut., 3 aut., 4 aut.); Graduate School of Oceanography, Univ. of Rhode Island/Narragansett/Etats-Unis (2 aut., 5 aut.)</AF>
<DT>Publication en série; Niveau analytique</DT>
<SO>Zeitschrift für Geomorphologie; ISSN 0372-8854; Coden ZGMPAG; Allemagne; Da. 2013; Vol. 57; No. 3 Suppl.; Pp. 125-137; Bibl. 29 ref.; 12 fig.</SO>
<LA>Anglais</LA>
<EA>This paper reports the results of the Remotely Operated Vehicle (ROV) exploration combined with multibeam data, providing new information about the main morphological characteristics of the Nisyros submarine volcanic centres. ROV exploration of the eastern flank of Yali revealed wave-type sediment structures, as well as linear fractures at various depths. Several smaller craters were also discovered on the northwest slopes of Strongyli, aligned with ENE-WSW trending fractures with no signs of hydrothermal activity. Heavy biogenic encrustations cover the volcanic rock outcrops on the flanks of both Yali and Strongyli. Analysis of recovered samples will provide information about their relationship to the geology of the nearby islands.</EA>
<CC>53186; 531</CC>
<FD>Fond sous-marin; Géomorphologie sous-marine; Volcan; Volcanisme; Quaternaire; Bathymétrie; Néotectonique; Fossé tectonique; Stratigraphie; Grèce; Méditerranée; Egée mer</FD>
<ED>Sea floor; Submarine geomorphology; Volcano; Volcanism; Quaternary; Bathymetry; Neotectonics; Graben; Stratigraphy; Greece; Mediterranean Sea; Aegean Sea</ED>
<SD>Fondo submarino; Geomorfología submarina; Volcán; Volcanismo; Cuaternario; Batimetría; Neotectónica; Foso tectónico; Estratigrafía; Grecia; El Mediterranéo; Mar Egeo</SD>
<LO>INIST-8829</LO>
<ID>28016309</ID>
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Exploring the Avyssos-Yali-Strogyli submarine volcanic complex at the eastern edge of the Aegean Volcanic Arc

Exploring the Avyssos-Yali-Strogyli submarine volcanic complex at the eastern edge of the Aegean Volcanic Arc

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