Neotectonics and the Kos Plateau Tuff eruption of 161 ka, South Aegean arc
Identifieur interne : 000028 ( PascalFrancis/Checkpoint ); précédent : 000027; suivant : 000029Neotectonics 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.
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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Box 1006</s1><s2>Dartmouth, Nova Scotia, B2Y 4A2</s2><s3>CAN</s3><sZ>2 aut.</sZ></inist:fA14><country>Canada</country><wicri:noRegion>Dartmouth, Nova Scotia, B2Y 4A2</wicri:noRegion></affiliation></author><author><name sortKey="Perissoratis, Constantine" sort="Perissoratis, Constantine" uniqKey="Perissoratis C" first="Constantine" last="Perissoratis">Constantine Perissoratis</name><affiliation wicri:level="1"><inist: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></inist:fA14><country>Grèce</country><placeName><settlement type="city">Athènes</settlement><region nuts="2" type="region">Attique (région)</region></placeName></affiliation></author></titleStmt><publicationStmt><idno type="wicri:source">INIST</idno><idno type="inist">05-0458213</idno><date when="2005">2005</date><idno type="stanalyst">PASCAL 05-0458213 INIST</idno><idno type="RBID">Pascal:05-0458213</idno><idno type="wicri:Area/PascalFrancis/Corpus">000027</idno><idno type="wicri:Area/PascalFrancis/Curation">000013</idno><idno type="wicri:Area/PascalFrancis/Checkpoint">000028</idno><idno type="wicri:explorRef" wicri:stream="PascalFrancis" wicri:step="Checkpoint">000028</idno></publicationStmt><sourceDesc><biblStruct><analytic><title xml:lang="en" level="a">Neotectonics and the Kos Plateau Tuff eruption of 161 ka, South Aegean arc</title><author><name sortKey="Pe Piper, Georgia" sort="Pe Piper, Georgia" uniqKey="Pe Piper G" first="Georgia" last="Pe-Piper">Georgia Pe-Piper</name><affiliation wicri:level="1"><inist: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></inist:fA14><country>Canada</country><wicri:noRegion>Halifax, Nova Scotia, B3H 3C3</wicri:noRegion></affiliation></author><author><name sortKey="Piper, David J W" sort="Piper, David J W" uniqKey="Piper D" first="David J. W." last="Piper">David J. W. Piper</name><affiliation wicri:level="1"><inist: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></inist:fA14><country>Canada</country><wicri:noRegion>Dartmouth, Nova Scotia, B2Y 4A2</wicri:noRegion></affiliation></author><author><name sortKey="Perissoratis, Constantine" sort="Perissoratis, Constantine" uniqKey="Perissoratis C" first="Constantine" last="Perissoratis">Constantine Perissoratis</name><affiliation wicri:level="1"><inist: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></inist:fA14><country>Grèce</country><placeName><settlement type="city">Athènes</settlement><region nuts="2" type="region">Attique (région)</region></placeName></affiliation></author></analytic><series><title level="j" type="main">Journal of volcanology and geothermal research</title><title level="j" type="abbreviated">J. volcanol. geotherm. res.</title><idno type="ISSN">0377-0273</idno><imprint><date when="2005">2005</date></imprint></series></biblStruct></sourceDesc><seriesStmt><title level="j" type="main">Journal of volcanology and geothermal research</title><title level="j" type="abbreviated">J. volcanol. geotherm. res.</title><idno type="ISSN">0377-0273</idno></seriesStmt></fileDesc><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></keywords><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></keywords></textClass></profileDesc></teiHeader><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></front></TEI><inist><standard h6="B"><pA><fA01 i1="01" i2="1"><s0>0377-0273</s0></fA01><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. 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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" 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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><affiliations><list><country><li>Canada</li><li>Grèce</li></country><region><li>Attique (région)</li></region><settlement><li>Athènes</li></settlement></list><tree><country name="Canada"><noRegion><name sortKey="Pe Piper, Georgia" sort="Pe Piper, Georgia" uniqKey="Pe Piper G" first="Georgia" last="Pe-Piper">Georgia Pe-Piper</name></noRegion><name sortKey="Piper, David J W" sort="Piper, David J W" uniqKey="Piper D" first="David J. W." last="Piper">David J. W. Piper</name></country><country name="Grèce"><region name="Attique (région)"><name sortKey="Perissoratis, Constantine" sort="Perissoratis, Constantine" uniqKey="Perissoratis C" first="Constantine" last="Perissoratis">Constantine Perissoratis</name></region></country></tree></affiliations></record>Pour manipuler ce document sous Unix (Dilib)
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|wiki= Wicri/Terre
|area= NissirosV1
|flux= PascalFrancis
|étape= Checkpoint
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|clé= Pascal:05-0458213
|texte= Neotectonics and the Kos Plateau Tuff eruption of 161 ka, South Aegean arc
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