NissirosV1, PascalFrancis, Curation, bibRecord, 000013

Neotectonics and the Kos Plateau Tuff eruption of 161 ka, South Aegean arc

Identifieur interne : 000013 ( PascalFrancis/Curation ); précédent : 000012; suivant : 000014

Neotectonics and the Kos Plateau Tuff eruption of 161 ka, South Aegean arc

Auteurs : Georgia Pe-Piper [Canada] ; David J. W. Piper [Canada] ; Constantine Perissoratis [Grèce]

Source :

Journal of volcanology and geothermal research [ 0377-0273 ] ; 2005.

RBID : Pascal:05-0458213

Descripteurs français

Pascal (Inist)
- Néotectonique, Ile Cos, Arc volcanique, Hellénides, Eruption, Tuf volcanique, Pléistocène, Levé sismique, Sismique réflexion, Haute résolution, Subsidence, Sédiment marin, Off shore, Discordance, Surface érosion, Transgression, Eustatisme, Taux sédimentation, Milieu eau peu profonde, Plaine côtière, Coulée pyroclastique, Explosion, Composition rhyolitique, Bassin Cos, Ile Pachia, Ile Pyrgousa, Ile Tilos, Ile Nisyros, Dacite, Linéament, Profil sismique, Faille.

English descriptors

KwdEn :
- Hellenides, Kos, Pleistocene, coastal plains, dacites, erosion surfaces, eruptions, eustacy, explosions, faults, high resolution, lineaments, marine sediments, neotectonics, offshore, pyroclastic flows, rhyolitic composition, sedimentation rates, seismic profiles, seismic reflection, seismic surveys, shallow-water environment, subsidence, transgression, tuff, unconformities, volcanic arcs.

Abstract

A high-resolution seismic-reflection survey of the area between Kos and Tilos islands is used to constrain the nature of the Kos Plateau Tuff (KPT) eruption and post-eruptive subsidence. A unique acoustically incoherent unit tens of metres thick at a subbottom depth of 15-35 m is recognised throughout the West Kos basin, which lies between Pachia, Yali and Kos. It commonly unconformably overlies folded, stratified sediment, but in places is concordant with stratified sediment more than 100 m thick. In places south of Kos, the acoustically incoherent unit is overlain by an unconformity and irregularly stratified sediment interpreted as terrestrial or shallow marine. Southeast of Nisyros, a correlative acoustically incoherent unit overlies a planar marine transgression erosion surface that extends almost to Tilos. The stratigraphic level of this unit is dated by comparison with the global eustatic sea-level record and the presence of major transgressive erosion surfaces on adjacent continental shelves, constrained by regional sedimentation rates, and indicates that it is of similar age to the Kos Plateau Tuff eruption. The relationship of this unit to coastal erosion surfaces, and its absence in many areas where seismic-reflection profiles show continuous marine sedimentation, suggests that it is a pyroclastic deposit of subaerial, or at most very shallow marine, origin from the Kos Plateau Tuff eruption. This presence of transgressive unconformities implies that a coastal plain or shallow sea extended southeast of Nisyros to Tilos and the Datça peninsula, and thus it is unlikely that pyroclastic flows crossed large stretches of deep water towards Tilos, as proposed by Allen and Cas (Allen, S.R., Cas, R.A.F., 2001. Transport of pyroclastic flows across the sea during the explosive, rhyolitic eruption of the Kos Plateau Tuff, Greece. Bull. Volcanol. 62, 441-456).

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A08	`01`	`1`	`ENG`	`@1 Neotectonics and the Kos Plateau Tuff eruption of 161 ka, South Aegean arc`
A11	`01`	`1`		`@1 PE-PIPER (Georgia)`
A11	`02`	`1`		`@1 PIPER (David J. W.)`
A11	`03`	`1`		`@1 PERISSORATIS (Constantine)`
A14	`01`			`@1 Department of Geology, Saint Mary's University @2 Halifax, Nova Scotia, B3H 3C3 @3 CAN @Z 1 aut.`
A14	`02`			`@1 Geological Survey of Canada (Atlantic), Bedford Institute of Oceanography, P.O. Box 1006 @2 Dartmouth, Nova Scotia, B2Y 4A2 @3 CAN @Z 2 aut.`
A14	`03`			`@1 Institute of Geology and Mineral Exploration, 70 Messoghion Street @2 11527 Athens @3 GRC @Z 3 aut.`
A20				`@1 315-338`
A21				`@1 2005`
A23	`01`			`@0 ENG`
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A44				`@0 0000 @1 © 2005 INIST-CNRS. All rights reserved.`
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C01	`01`		`ENG`	@0 A high-resolution seismic-reflection survey of the area between Kos and Tilos islands is used to constrain the nature of the Kos Plateau Tuff (KPT) eruption and post-eruptive subsidence. A unique acoustically incoherent unit tens of metres thick at a subbottom depth of 15-35 m is recognised throughout the West Kos basin, which lies between Pachia, Yali and Kos. It commonly unconformably overlies folded, stratified sediment, but in places is concordant with stratified sediment more than 100 m thick. In places south of Kos, the acoustically incoherent unit is overlain by an unconformity and irregularly stratified sediment interpreted as terrestrial or shallow marine. Southeast of Nisyros, a correlative acoustically incoherent unit overlies a planar marine transgression erosion surface that extends almost to Tilos. The stratigraphic level of this unit is dated by comparison with the global eustatic sea-level record and the presence of major transgressive erosion surfaces on adjacent continental shelves, constrained by regional sedimentation rates, and indicates that it is of similar age to the Kos Plateau Tuff eruption. The relationship of this unit to coastal erosion surfaces, and its absence in many areas where seismic-reflection profiles show continuous marine sedimentation, suggests that it is a pyroclastic deposit of subaerial, or at most very shallow marine, origin from the Kos Plateau Tuff eruption. This presence of transgressive unconformities implies that a coastal plain or shallow sea extended southeast of Nisyros to Tilos and the Datça peninsula, and thus it is unlikely that pyroclastic flows crossed large stretches of deep water towards Tilos, as proposed by Allen and Cas (Allen, S.R., Cas, R.A.F., 2001. Transport of pyroclastic flows across the sea during the explosive, rhyolitic eruption of the Kos Plateau Tuff, Greece. Bull. Volcanol. 62, 441-456).
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C02	`05`	`2`		`@0 001E01L`
C02	`06`	`2`		`@0 001E01P02`
C03	`01`	`2`	`FRE`	`@0 Néotectonique @5 01`
C03	`01`	`2`	`ENG`	`@0 neotectonics @5 01`
C03	`01`	`2`	`SPA`	`@0 Neotectónico @5 01`
C03	`02`	`2`	`FRE`	`@0 Ile Cos @2 NG @5 02`
C03	`02`	`2`	`ENG`	`@0 Kos @2 NG @5 02`
C03	`02`	`2`	`SPA`	`@0 Isla Cos @2 NG @5 02`
C03	`03`	`2`	`FRE`	`@0 Arc volcanique @5 04`
C03	`03`	`2`	`ENG`	`@0 volcanic arcs @5 04`
C03	`04`	`2`	`FRE`	`@0 Hellénides @2 NG @5 05`
C03	`04`	`2`	`ENG`	`@0 Hellenides @2 NG @5 05`
C03	`05`	`2`	`FRE`	`@0 Eruption @5 06`
C03	`05`	`2`	`ENG`	`@0 eruptions @5 06`
C03	`05`	`2`	`SPA`	`@0 Erupción @5 06`
C03	`06`	`2`	`FRE`	`@0 Tuf volcanique @2 NV @5 07`
C03	`06`	`2`	`ENG`	`@0 tuff @2 NV @5 07`
C03	`06`	`2`	`SPA`	`@0 Toba volcánica @2 NV @5 07`
C03	`07`	`2`	`FRE`	`@0 Pléistocène @2 NX @5 09`
C03	`07`	`2`	`ENG`	`@0 Pleistocene @2 NX @5 09`
C03	`08`	`2`	`FRE`	`@0 Levé sismique @5 10`
C03	`08`	`2`	`ENG`	`@0 seismic surveys @5 10`
C03	`08`	`2`	`SPA`	`@0 Levantamiento sísmico @5 10`
C03	`09`	`2`	`FRE`	`@0 Sismique réflexion @5 11`
C03	`09`	`2`	`ENG`	`@0 seismic reflection @5 11`
C03	`09`	`2`	`SPA`	`@0 Método reflexión sísmica @5 11`
C03	`10`	`2`	`FRE`	`@0 Haute résolution @5 12`
C03	`10`	`2`	`ENG`	`@0 high resolution @5 12`
C03	`10`	`2`	`SPA`	`@0 Alta resolucion @5 12`
C03	`11`	`2`	`FRE`	`@0 Subsidence @5 13`
C03	`11`	`2`	`ENG`	`@0 subsidence @5 13`
C03	`11`	`2`	`SPA`	`@0 Subsidencia @5 13`
C03	`12`	`2`	`FRE`	`@0 Sédiment marin @5 14`
C03	`12`	`2`	`ENG`	`@0 marine sediments @5 14`
C03	`12`	`2`	`SPA`	`@0 Sedimento marino @5 14`
C03	`13`	`2`	`FRE`	`@0 Off shore @5 15`
C03	`13`	`2`	`ENG`	`@0 offshore @5 15`
C03	`13`	`2`	`SPA`	`@0 Off shore @5 15`
C03	`14`	`2`	`FRE`	`@0 Discordance @5 16`
C03	`14`	`2`	`ENG`	`@0 unconformities @5 16`
C03	`14`	`2`	`SPA`	`@0 Discordancia @5 16`
C03	`15`	`2`	`FRE`	`@0 Surface érosion @5 17`
C03	`15`	`2`	`ENG`	`@0 erosion surfaces @5 17`
C03	`15`	`2`	`SPA`	`@0 Superficie erosión @5 17`
C03	`16`	`2`	`FRE`	`@0 Transgression @5 18`
C03	`16`	`2`	`ENG`	`@0 transgression @5 18`
C03	`16`	`2`	`SPA`	`@0 Transgresión @5 18`
C03	`17`	`2`	`FRE`	`@0 Eustatisme @5 19`
C03	`17`	`2`	`ENG`	`@0 eustacy @5 19`
C03	`17`	`2`	`SPA`	`@0 Eustasia @5 19`
C03	`18`	`2`	`FRE`	`@0 Taux sédimentation @5 20`
C03	`18`	`2`	`ENG`	`@0 sedimentation rates @5 20`
C03	`18`	`2`	`SPA`	`@0 Proporción material sedimentado @5 20`
C03	`19`	`2`	`FRE`	`@0 Milieu eau peu profonde @5 21`
C03	`19`	`2`	`ENG`	`@0 shallow-water environment @5 21`
C03	`19`	`2`	`SPA`	`@0 Medio agua poco profunda @5 21`
C03	`20`	`2`	`FRE`	`@0 Plaine côtière @5 22`
C03	`20`	`2`	`ENG`	`@0 coastal plains @5 22`
C03	`20`	`2`	`SPA`	`@0 Planicie costera @5 22`
C03	`21`	`2`	`FRE`	`@0 Coulée pyroclastique @5 23`
C03	`21`	`2`	`ENG`	`@0 pyroclastic flows @5 23`
C03	`22`	`2`	`FRE`	`@0 Explosion @5 24`
C03	`22`	`2`	`ENG`	`@0 explosions @5 24`
C03	`22`	`2`	`SPA`	`@0 Explosión @5 24`
C03	`23`	`2`	`FRE`	`@0 Composition rhyolitique @5 25`
C03	`23`	`2`	`ENG`	`@0 rhyolitic composition @5 25`
C03	`23`	`2`	`SPA`	`@0 Composición riolítica @5 25`
C03	`24`	`2`	`FRE`	`@0 Bassin Cos @4 INC @5 52`
C03	`25`	`2`	`FRE`	`@0 Ile Pachia @4 INC @5 53`
C03	`26`	`2`	`FRE`	`@0 Ile Pyrgousa @4 INC @5 54`
C03	`27`	`2`	`FRE`	`@0 Ile Tilos @4 INC @5 55`
C03	`28`	`2`	`FRE`	`@0 Ile Nisyros @4 INC @5 56`
C03	`29`	`2`	`FRE`	`@0 Dacite @2 NV @5 61`
C03	`29`	`2`	`ENG`	`@0 dacites @2 NV @5 61`
C03	`29`	`2`	`SPA`	`@0 Dacita @2 NV @5 61`
C03	`30`	`2`	`FRE`	`@0 Linéament @5 62`
C03	`30`	`2`	`ENG`	`@0 lineaments @5 62`
C03	`30`	`2`	`SPA`	`@0 Lineamento @5 62`
C03	`31`	`2`	`FRE`	`@0 Profil sismique @5 63`
C03	`31`	`2`	`ENG`	`@0 seismic profiles @5 63`
C03	`32`	`2`	`FRE`	`@0 Faille @5 64`
C03	`32`	`2`	`ENG`	`@0 faults @5 64`
C03	`32`	`2`	`SPA`	`@0 Quebrado @5 64`
C06				`@0 ILS`
C07	`01`	`2`	`FRE`	`@0 Iles Dodécanèse @2 NG`
C07	`01`	`2`	`ENG`	`@0 Dodecanese @2 NG`
C07	`01`	`2`	`SPA`	`@0 Islas Dodecanese @2 NG`
C07	`02`	`2`	`FRE`	`@0 Iles Egée Grèce @2 NG`
C07	`02`	`2`	`ENG`	`@0 Greek Aegean Islands @2 NG`
C07	`02`	`2`	`SPA`	`@0 Islas Egeas Griegas @2 NG`
C07	`03`	`2`	`FRE`	`@0 Grèce @2 NG`
C07	`03`	`2`	`ENG`	`@0 Greece @2 NG`
C07	`03`	`2`	`SPA`	`@0 Grecia @2 NG`
C07	`04`	`2`	`FRE`	`@0 Europe Sud @2 NG`
C07	`04`	`2`	`ENG`	`@0 Southern Europe @2 NG`
C07	`04`	`2`	`SPA`	`@0 Europa Sur @2 NG`
C07	`05`	`2`	`FRE`	`@0 Europe`
C07	`05`	`2`	`ENG`	`@0 Europe`
C07	`05`	`2`	`SPA`	`@0 Europa`
C07	`06`	`2`	`FRE`	`@0 Pyroclastite @2 NV`
C07	`06`	`2`	`ENG`	`@0 pyroclastics @2 NV`
C07	`07`	`2`	`FRE`	`@0 Roche volcanique @2 NV`
C07	`07`	`2`	`ENG`	`@0 volcanic rocks @2 NV`
C07	`07`	`2`	`SPA`	`@0 Roca volcánica @2 NV`
C07	`08`	`2`	`FRE`	`@0 Roche ignée`
C07	`08`	`2`	`ENG`	`@0 igneous rocks`
C07	`08`	`2`	`SPA`	`@0 Roca ignea`
C07	`09`	`2`	`FRE`	`@0 Quaternaire @2 NX`
C07	`09`	`2`	`ENG`	`@0 Quaternary @2 NX`
C07	`09`	`2`	`SPA`	`@0 Cuaternario @2 NX`
C07	`10`	`2`	`FRE`	`@0 Cénozoïque @2 NX`
C07	`10`	`2`	`ENG`	`@0 Cenozoic @2 NX`
C07	`10`	`2`	`SPA`	`@0 Cenozoico @2 NX`
C07	`11`	`2`	`FRE`	`@0 Phanérozoïque`
C07	`11`	`2`	`ENG`	`@0 Phanerozoic`
C07	`11`	`2`	`SPA`	`@0 Fanerozoico`
N21				`@1 318`
N44	`01`			`@1 PSI`
N82				`@1 PSI`

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Le document en format XML

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<author><name sortKey="Perissoratis, Constantine" sort="Perissoratis, Constantine" uniqKey="Perissoratis C" first="Constantine" last="Perissoratis">Constantine Perissoratis</name>
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<author><name sortKey="Perissoratis, Constantine" sort="Perissoratis, Constantine" uniqKey="Perissoratis C" first="Constantine" last="Perissoratis">Constantine Perissoratis</name>
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<profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>Hellenides</term>
<term>Kos</term>
<term>Pleistocene</term>
<term>coastal plains</term>
<term>dacites</term>
<term>erosion surfaces</term>
<term>eruptions</term>
<term>eustacy</term>
<term>explosions</term>
<term>faults</term>
<term>high resolution</term>
<term>lineaments</term>
<term>marine sediments</term>
<term>neotectonics</term>
<term>offshore</term>
<term>pyroclastic flows</term>
<term>rhyolitic composition</term>
<term>sedimentation rates</term>
<term>seismic profiles</term>
<term>seismic reflection</term>
<term>seismic surveys</term>
<term>shallow-water environment</term>
<term>subsidence</term>
<term>transgression</term>
<term>tuff</term>
<term>unconformities</term>
<term>volcanic arcs</term>
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<keywords scheme="Pascal" xml:lang="fr"><term>Néotectonique</term>
<term>Ile Cos</term>
<term>Arc volcanique</term>
<term>Hellénides</term>
<term>Eruption</term>
<term>Tuf volcanique</term>
<term>Pléistocène</term>
<term>Levé sismique</term>
<term>Sismique réflexion</term>
<term>Haute résolution</term>
<term>Subsidence</term>
<term>Sédiment marin</term>
<term>Off shore</term>
<term>Discordance</term>
<term>Surface érosion</term>
<term>Transgression</term>
<term>Eustatisme</term>
<term>Taux sédimentation</term>
<term>Milieu eau peu profonde</term>
<term>Plaine côtière</term>
<term>Coulée pyroclastique</term>
<term>Explosion</term>
<term>Composition rhyolitique</term>
<term>Bassin Cos</term>
<term>Ile Pachia</term>
<term>Ile Pyrgousa</term>
<term>Ile Tilos</term>
<term>Ile Nisyros</term>
<term>Dacite</term>
<term>Linéament</term>
<term>Profil sismique</term>
<term>Faille</term>
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<front><div type="abstract" xml:lang="en">A high-resolution seismic-reflection survey of the area between Kos and Tilos islands is used to constrain the nature of the Kos Plateau Tuff (KPT) eruption and post-eruptive subsidence. A unique acoustically incoherent unit tens of metres thick at a subbottom depth of 15-35 m is recognised throughout the West Kos basin, which lies between Pachia, Yali and Kos. It commonly unconformably overlies folded, stratified sediment, but in places is concordant with stratified sediment more than 100 m thick. In places south of Kos, the acoustically incoherent unit is overlain by an unconformity and irregularly stratified sediment interpreted as terrestrial or shallow marine. Southeast of Nisyros, a correlative acoustically incoherent unit overlies a planar marine transgression erosion surface that extends almost to Tilos. The stratigraphic level of this unit is dated by comparison with the global eustatic sea-level record and the presence of major transgressive erosion surfaces on adjacent continental shelves, constrained by regional sedimentation rates, and indicates that it is of similar age to the Kos Plateau Tuff eruption. The relationship of this unit to coastal erosion surfaces, and its absence in many areas where seismic-reflection profiles show continuous marine sedimentation, suggests that it is a pyroclastic deposit of subaerial, or at most very shallow marine, origin from the Kos Plateau Tuff eruption. This presence of transgressive unconformities implies that a coastal plain or shallow sea extended southeast of Nisyros to Tilos and the Datça peninsula, and thus it is unlikely that pyroclastic flows crossed large stretches of deep water towards Tilos, as proposed by Allen and Cas (Allen, S.R., Cas, R.A.F., 2001. Transport of pyroclastic flows across the sea during the explosive, rhyolitic eruption of the Kos Plateau Tuff, Greece. Bull. Volcanol. 62, 441-456).</div>
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<fA02 i1="01"><s0>JVGRDQ</s0>
</fA02>
<fA03 i2="1"><s0>J. volcanol. geotherm. res.</s0>
</fA03>
<fA05><s2>139</s2>
</fA05>
<fA06><s2>3-4</s2>
</fA06>
<fA08 i1="01" i2="1" l="ENG"><s1>Neotectonics and the Kos Plateau Tuff eruption of 161 ka, South Aegean arc</s1>
</fA08>
<fA11 i1="01" i2="1"><s1>PE-PIPER (Georgia)</s1>
</fA11>
<fA11 i1="02" i2="1"><s1>PIPER (David J. W.)</s1>
</fA11>
<fA11 i1="03" i2="1"><s1>PERISSORATIS (Constantine)</s1>
</fA11>
<fA14 i1="01"><s1>Department of Geology, Saint Mary's University</s1>
<s2>Halifax, Nova Scotia, B3H 3C3</s2>
<s3>CAN</s3>
<sZ>1 aut.</sZ>
</fA14>
<fA14 i1="02"><s1>Geological Survey of Canada (Atlantic), Bedford Institute of Oceanography, P.O. Box 1006</s1>
<s2>Dartmouth, Nova Scotia, B2Y 4A2</s2>
<s3>CAN</s3>
<sZ>2 aut.</sZ>
</fA14>
<fA14 i1="03"><s1>Institute of Geology and Mineral Exploration, 70 Messoghion Street</s1>
<s2>11527 Athens</s2>
<s3>GRC</s3>
<sZ>3 aut.</sZ>
</fA14>
<fA20><s1>315-338</s1>
</fA20>
<fA21><s1>2005</s1>
</fA21>
<fA23 i1="01"><s0>ENG</s0>
</fA23>
<fA43 i1="01"><s1>INIST</s1>
<s2>17236</s2>
<s5>354000126034790100</s5>
</fA43>
<fA44><s0>0000</s0>
<s1>© 2005 INIST-CNRS. All rights reserved.</s1>
</fA44>
<fA45><s0>1 p.1/2</s0>
</fA45>
<fA47 i1="01" i2="1"><s0>05-0458213</s0>
</fA47>
<fA60><s1>P</s1>
</fA60>
<fA61><s0>A</s0>
</fA61>
<fA64 i1="01" i2="1"><s0>Journal of volcanology and geothermal research</s0>
</fA64>
<fA66 i1="01"><s0>NLD</s0>
</fA66>
<fC01 i1="01" l="ENG"><s0>A high-resolution seismic-reflection survey of the area between Kos and Tilos islands is used to constrain the nature of the Kos Plateau Tuff (KPT) eruption and post-eruptive subsidence. A unique acoustically incoherent unit tens of metres thick at a subbottom depth of 15-35 m is recognised throughout the West Kos basin, which lies between Pachia, Yali and Kos. It commonly unconformably overlies folded, stratified sediment, but in places is concordant with stratified sediment more than 100 m thick. In places south of Kos, the acoustically incoherent unit is overlain by an unconformity and irregularly stratified sediment interpreted as terrestrial or shallow marine. Southeast of Nisyros, a correlative acoustically incoherent unit overlies a planar marine transgression erosion surface that extends almost to Tilos. The stratigraphic level of this unit is dated by comparison with the global eustatic sea-level record and the presence of major transgressive erosion surfaces on adjacent continental shelves, constrained by regional sedimentation rates, and indicates that it is of similar age to the Kos Plateau Tuff eruption. The relationship of this unit to coastal erosion surfaces, and its absence in many areas where seismic-reflection profiles show continuous marine sedimentation, suggests that it is a pyroclastic deposit of subaerial, or at most very shallow marine, origin from the Kos Plateau Tuff eruption. This presence of transgressive unconformities implies that a coastal plain or shallow sea extended southeast of Nisyros to Tilos and the Datça peninsula, and thus it is unlikely that pyroclastic flows crossed large stretches of deep water towards Tilos, as proposed by Allen and Cas (Allen, S.R., Cas, R.A.F., 2001. Transport of pyroclastic flows across the sea during the explosive, rhyolitic eruption of the Kos Plateau Tuff, Greece. Bull. Volcanol. 62, 441-456).</s0>
</fC01>
<fC02 i1="01" i2="2"><s0>222A01</s0>
</fC02>
<fC02 i1="02" i2="2"><s0>225A</s0>
</fC02>
<fC02 i1="03" i2="2"><s0>226C02</s0>
</fC02>
<fC02 i1="04" i2="2"><s0>001E01F01</s0>
</fC02>
<fC02 i1="05" i2="2"><s0>001E01L</s0>
</fC02>
<fC02 i1="06" i2="2"><s0>001E01P02</s0>
</fC02>
<fC03 i1="01" i2="2" l="FRE"><s0>Néotectonique</s0>
<s5>01</s5>
</fC03>
<fC03 i1="01" i2="2" l="ENG"><s0>neotectonics</s0>
<s5>01</s5>
</fC03>
<fC03 i1="01" i2="2" l="SPA"><s0>Neotectónico</s0>
<s5>01</s5>
</fC03>
<fC03 i1="02" i2="2" l="FRE"><s0>Ile Cos</s0>
<s2>NG</s2>
<s5>02</s5>
</fC03>
<fC03 i1="02" i2="2" l="ENG"><s0>Kos</s0>
<s2>NG</s2>
<s5>02</s5>
</fC03>
<fC03 i1="02" i2="2" l="SPA"><s0>Isla Cos</s0>
<s2>NG</s2>
<s5>02</s5>
</fC03>
<fC03 i1="03" i2="2" l="FRE"><s0>Arc volcanique</s0>
<s5>04</s5>
</fC03>
<fC03 i1="03" i2="2" l="ENG"><s0>volcanic arcs</s0>
<s5>04</s5>
</fC03>
<fC03 i1="04" i2="2" l="FRE"><s0>Hellénides</s0>
<s2>NG</s2>
<s5>05</s5>
</fC03>
<fC03 i1="04" i2="2" l="ENG"><s0>Hellenides</s0>
<s2>NG</s2>
<s5>05</s5>
</fC03>
<fC03 i1="05" i2="2" l="FRE"><s0>Eruption</s0>
<s5>06</s5>
</fC03>
<fC03 i1="05" i2="2" l="ENG"><s0>eruptions</s0>
<s5>06</s5>
</fC03>
<fC03 i1="05" i2="2" l="SPA"><s0>Erupción</s0>
<s5>06</s5>
</fC03>
<fC03 i1="06" i2="2" l="FRE"><s0>Tuf volcanique</s0>
<s2>NV</s2>
<s5>07</s5>
</fC03>
<fC03 i1="06" i2="2" l="ENG"><s0>tuff</s0>
<s2>NV</s2>
<s5>07</s5>
</fC03>
<fC03 i1="06" i2="2" l="SPA"><s0>Toba volcánica</s0>
<s2>NV</s2>
<s5>07</s5>
</fC03>
<fC03 i1="07" i2="2" l="FRE"><s0>Pléistocène</s0>
<s2>NX</s2>
<s5>09</s5>
</fC03>
<fC03 i1="07" i2="2" l="ENG"><s0>Pleistocene</s0>
<s2>NX</s2>
<s5>09</s5>
</fC03>
<fC03 i1="08" i2="2" l="FRE"><s0>Levé sismique</s0>
<s5>10</s5>
</fC03>
<fC03 i1="08" i2="2" l="ENG"><s0>seismic surveys</s0>
<s5>10</s5>
</fC03>
<fC03 i1="08" i2="2" l="SPA"><s0>Levantamiento sísmico</s0>
<s5>10</s5>
</fC03>
<fC03 i1="09" i2="2" l="FRE"><s0>Sismique réflexion</s0>
<s5>11</s5>
</fC03>
<fC03 i1="09" i2="2" l="ENG"><s0>seismic reflection</s0>
<s5>11</s5>
</fC03>
<fC03 i1="09" i2="2" l="SPA"><s0>Método reflexión sísmica</s0>
<s5>11</s5>
</fC03>
<fC03 i1="10" i2="2" l="FRE"><s0>Haute résolution</s0>
<s5>12</s5>
</fC03>
<fC03 i1="10" i2="2" l="ENG"><s0>high resolution</s0>
<s5>12</s5>
</fC03>
<fC03 i1="10" i2="2" l="SPA"><s0>Alta resolucion</s0>
<s5>12</s5>
</fC03>
<fC03 i1="11" i2="2" l="FRE"><s0>Subsidence</s0>
<s5>13</s5>
</fC03>
<fC03 i1="11" i2="2" l="ENG"><s0>subsidence</s0>
<s5>13</s5>
</fC03>
<fC03 i1="11" i2="2" l="SPA"><s0>Subsidencia</s0>
<s5>13</s5>
</fC03>
<fC03 i1="12" i2="2" l="FRE"><s0>Sédiment marin</s0>
<s5>14</s5>
</fC03>
<fC03 i1="12" i2="2" l="ENG"><s0>marine sediments</s0>
<s5>14</s5>
</fC03>
<fC03 i1="12" i2="2" l="SPA"><s0>Sedimento marino</s0>
<s5>14</s5>
</fC03>
<fC03 i1="13" i2="2" l="FRE"><s0>Off shore</s0>
<s5>15</s5>
</fC03>
<fC03 i1="13" i2="2" l="ENG"><s0>offshore</s0>
<s5>15</s5>
</fC03>
<fC03 i1="13" i2="2" l="SPA"><s0>Off shore</s0>
<s5>15</s5>
</fC03>
<fC03 i1="14" i2="2" l="FRE"><s0>Discordance</s0>
<s5>16</s5>
</fC03>
<fC03 i1="14" i2="2" l="ENG"><s0>unconformities</s0>
<s5>16</s5>
</fC03>
<fC03 i1="14" i2="2" l="SPA"><s0>Discordancia</s0>
<s5>16</s5>
</fC03>
<fC03 i1="15" i2="2" l="FRE"><s0>Surface érosion</s0>
<s5>17</s5>
</fC03>
<fC03 i1="15" i2="2" l="ENG"><s0>erosion surfaces</s0>
<s5>17</s5>
</fC03>
<fC03 i1="15" i2="2" l="SPA"><s0>Superficie erosión</s0>
<s5>17</s5>
</fC03>
<fC03 i1="16" i2="2" l="FRE"><s0>Transgression</s0>
<s5>18</s5>
</fC03>
<fC03 i1="16" i2="2" l="ENG"><s0>transgression</s0>
<s5>18</s5>
</fC03>
<fC03 i1="16" i2="2" l="SPA"><s0>Transgresión</s0>
<s5>18</s5>
</fC03>
<fC03 i1="17" i2="2" l="FRE"><s0>Eustatisme</s0>
<s5>19</s5>
</fC03>
<fC03 i1="17" i2="2" l="ENG"><s0>eustacy</s0>
<s5>19</s5>
</fC03>
<fC03 i1="17" i2="2" l="SPA"><s0>Eustasia</s0>
<s5>19</s5>
</fC03>
<fC03 i1="18" i2="2" l="FRE"><s0>Taux sédimentation</s0>
<s5>20</s5>
</fC03>
<fC03 i1="18" i2="2" l="ENG"><s0>sedimentation rates</s0>
<s5>20</s5>
</fC03>
<fC03 i1="18" i2="2" l="SPA"><s0>Proporción material sedimentado</s0>
<s5>20</s5>
</fC03>
<fC03 i1="19" i2="2" l="FRE"><s0>Milieu eau peu profonde</s0>
<s5>21</s5>
</fC03>
<fC03 i1="19" i2="2" l="ENG"><s0>shallow-water environment</s0>
<s5>21</s5>
</fC03>
<fC03 i1="19" i2="2" l="SPA"><s0>Medio agua poco profunda</s0>
<s5>21</s5>
</fC03>
<fC03 i1="20" i2="2" l="FRE"><s0>Plaine côtière</s0>
<s5>22</s5>
</fC03>
<fC03 i1="20" i2="2" l="ENG"><s0>coastal plains</s0>
<s5>22</s5>
</fC03>
<fC03 i1="20" i2="2" l="SPA"><s0>Planicie costera</s0>
<s5>22</s5>
</fC03>
<fC03 i1="21" i2="2" l="FRE"><s0>Coulée pyroclastique</s0>
<s5>23</s5>
</fC03>
<fC03 i1="21" i2="2" l="ENG"><s0>pyroclastic flows</s0>
<s5>23</s5>
</fC03>
<fC03 i1="22" i2="2" l="FRE"><s0>Explosion</s0>
<s5>24</s5>
</fC03>
<fC03 i1="22" i2="2" l="ENG"><s0>explosions</s0>
<s5>24</s5>
</fC03>
<fC03 i1="22" i2="2" l="SPA"><s0>Explosión</s0>
<s5>24</s5>
</fC03>
<fC03 i1="23" i2="2" l="FRE"><s0>Composition rhyolitique</s0>
<s5>25</s5>
</fC03>
<fC03 i1="23" i2="2" l="ENG"><s0>rhyolitic composition</s0>
<s5>25</s5>
</fC03>
<fC03 i1="23" i2="2" l="SPA"><s0>Composición riolítica</s0>
<s5>25</s5>
</fC03>
<fC03 i1="24" i2="2" l="FRE"><s0>Bassin Cos</s0>
<s4>INC</s4>
<s5>52</s5>
</fC03>
<fC03 i1="25" i2="2" l="FRE"><s0>Ile Pachia</s0>
<s4>INC</s4>
<s5>53</s5>
</fC03>
<fC03 i1="26" i2="2" l="FRE"><s0>Ile Pyrgousa</s0>
<s4>INC</s4>
<s5>54</s5>
</fC03>
<fC03 i1="27" i2="2" l="FRE"><s0>Ile Tilos</s0>
<s4>INC</s4>
<s5>55</s5>
</fC03>
<fC03 i1="28" i2="2" l="FRE"><s0>Ile Nisyros</s0>
<s4>INC</s4>
<s5>56</s5>
</fC03>
<fC03 i1="29" i2="2" l="FRE"><s0>Dacite</s0>
<s2>NV</s2>
<s5>61</s5>
</fC03>
<fC03 i1="29" i2="2" l="ENG"><s0>dacites</s0>
<s2>NV</s2>
<s5>61</s5>
</fC03>
<fC03 i1="29" i2="2" l="SPA"><s0>Dacita</s0>
<s2>NV</s2>
<s5>61</s5>
</fC03>
<fC03 i1="30" i2="2" l="FRE"><s0>Linéament</s0>
<s5>62</s5>
</fC03>
<fC03 i1="30" i2="2" l="ENG"><s0>lineaments</s0>
<s5>62</s5>
</fC03>
<fC03 i1="30" i2="2" l="SPA"><s0>Lineamento</s0>
<s5>62</s5>
</fC03>
<fC03 i1="31" i2="2" l="FRE"><s0>Profil sismique</s0>
<s5>63</s5>
</fC03>
<fC03 i1="31" i2="2" l="ENG"><s0>seismic profiles</s0>
<s5>63</s5>
</fC03>
<fC03 i1="32" i2="2" l="FRE"><s0>Faille</s0>
<s5>64</s5>
</fC03>
<fC03 i1="32" i2="2" l="ENG"><s0>faults</s0>
<s5>64</s5>
</fC03>
<fC03 i1="32" i2="2" l="SPA"><s0>Quebrado</s0>
<s5>64</s5>
</fC03>
<fC06><s0>ILS</s0>
</fC06>
<fC07 i1="01" i2="2" l="FRE"><s0>Iles Dodécanèse</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="01" i2="2" l="ENG"><s0>Dodecanese</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="01" i2="2" l="SPA"><s0>Islas Dodecanese</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="02" i2="2" l="FRE"><s0>Iles Egée Grèce</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="02" i2="2" l="ENG"><s0>Greek Aegean Islands</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="02" i2="2" l="SPA"><s0>Islas Egeas Griegas</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="03" i2="2" l="FRE"><s0>Grèce</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="03" i2="2" l="ENG"><s0>Greece</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="03" i2="2" l="SPA"><s0>Grecia</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="04" i2="2" l="FRE"><s0>Europe Sud</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="04" i2="2" l="ENG"><s0>Southern Europe</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="04" i2="2" l="SPA"><s0>Europa Sur</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="05" i2="2" l="FRE"><s0>Europe</s0>
</fC07>
<fC07 i1="05" i2="2" l="ENG"><s0>Europe</s0>
</fC07>
<fC07 i1="05" i2="2" l="SPA"><s0>Europa</s0>
</fC07>
<fC07 i1="06" i2="2" l="FRE"><s0>Pyroclastite</s0>
<s2>NV</s2>
</fC07>
<fC07 i1="06" i2="2" l="ENG"><s0>pyroclastics</s0>
<s2>NV</s2>
</fC07>
<fC07 i1="07" i2="2" l="FRE"><s0>Roche volcanique</s0>
<s2>NV</s2>
</fC07>
<fC07 i1="07" i2="2" l="ENG"><s0>volcanic rocks</s0>
<s2>NV</s2>
</fC07>
<fC07 i1="07" i2="2" l="SPA"><s0>Roca volcánica</s0>
<s2>NV</s2>
</fC07>
<fC07 i1="08" i2="2" l="FRE"><s0>Roche ignée</s0>
</fC07>
<fC07 i1="08" i2="2" l="ENG"><s0>igneous rocks</s0>
</fC07>
<fC07 i1="08" i2="2" l="SPA"><s0>Roca ignea</s0>
</fC07>
<fC07 i1="09" i2="2" l="FRE"><s0>Quaternaire</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="09" i2="2" l="ENG"><s0>Quaternary</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="09" i2="2" l="SPA"><s0>Cuaternario</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="10" i2="2" l="FRE"><s0>Cénozoïque</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="10" i2="2" l="ENG"><s0>Cenozoic</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="10" i2="2" l="SPA"><s0>Cenozoico</s0>
<s2>NX</s2>
</fC07>
<fC07 i1="11" i2="2" l="FRE"><s0>Phanérozoïque</s0>
</fC07>
<fC07 i1="11" i2="2" l="ENG"><s0>Phanerozoic</s0>
</fC07>
<fC07 i1="11" i2="2" l="SPA"><s0>Fanerozoico</s0>
</fC07>
<fN21><s1>318</s1>
</fN21>
<fN44 i1="01"><s1>PSI</s1>
</fN44>
<fN82><s1>PSI</s1>
</fN82>
</pA>
</standard>
</inist>
</record>

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Neotectonics and the Kos Plateau Tuff eruption of 161 ka, South Aegean arc

Neotectonics and the Kos Plateau Tuff eruption of 161 ka, South Aegean arc

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