LeHavreV1, PascalFrancis, Curation, bibRecord, 000235

Crustal seismic reflection measurements across the northern extension of the Taupo Volcanic Zone, North Island, New Zealand

Identifieur interne : 000235 ( PascalFrancis/Curation ); précédent : 000234; suivant : 000236

Crustal seismic reflection measurements across the northern extension of the Taupo Volcanic Zone, North Island, New Zealand

Auteurs : F. J. Davey [Nouvelle-Zélande]

Source :

Journal of volcanology and geothermal research [ 0377-0273 ] ; 2010.

RBID : Pascal:10-0252683

Descripteurs français

Pascal (Inist)
- Sismique réflexion, Extension, Off shore, Croûte terrestre inf, Manteau sup, Zone cisaillement, Sill, Réflecteur, Profondeur, Temps parcours, Fossé, Sismicité, Ecoulement, Plateau, Croûte terrestre, Manteau appauvri, Zone volcanique Taupo, Péninsule Raukumara.

English descriptors

KwdEn :
- Raukumara Peninsula, Taupo volcanic zone, crust, depleted mantle, depth, extension, flow, lower crust, offshore, plateaus, reflectors, seismic reflection, seismicity, shear zones, sills, travel time, troughs, upper mantle.

Abstract

A crustal seismic reflection profile across the offshore Taupo Volcanic Zone (OTVZ) has been reprocessed to improve the lower crust-upper mantle image. The OTVZ is underlain by several strong sub-horizontal crustal reflections that may correspond to shear zones or mafic sills. A reflector interpreted to correspond to Moho lies at a depth of about 8-8.5 s twt (seconds two-way-traveltime) - about 20 km - under the western margin of the Raukumara Peninsula and rises to a depth of about 6 s twt (about 16 km) under the active, eastern part of the OTVZ and can be traced at about this depth across most of the OTVZ. Underlying this inferred Moho are two diffuse zones of discontinuous reflectivity, one underlying the active eastern OTVZ and a less well defined one underlying the landward extension of the Havre Trough. They extend from about 15 to 35 km depth, within the mantle wedge, and are inferred to be imaging a zone of depleted upper mantle associated with crustal extension. A localised zone of deep (30-50 km) reflectivity and seismicity occurs under the eastern OTVZ margin and may relate to fluid flow from the Hikurangi plateau being subducted further east.

A01	`01`	`1`		`@0 0377-0273`
A02	`01`			`@0 JVGRDQ`
A03		`1`		`@0 J. volcanol. geotherm. res.`
A05				`@2 190`
A06				`@2 1-2`
A08	`01`	`1`	`ENG`	`@1 Crustal seismic reflection measurements across the northern extension of the Taupo Volcanic Zone, North Island, New Zealand`
A09	`01`	`1`	`ENG`	`@1 Making and Breaking the Arc: A Volume in Honour of Professor John Gamble`
A11	`01`	`1`		`@1 DAVEY (F. J.)`
A12	`01`	`1`		`@1 WYSOCZANSKI (Richard J.) @9 ed.`
A12	`02`	`1`		`@1 ROWLAND (Julie V.) @9 ed.`
A12	`03`	`1`		`@1 BEKER (Joel A.) @9 ed.`
A12	`04`	`1`		`@1 WILSON (Colin J. N.) @9 ed.`
A14	`01`			`@1 GNS Science, PO Box 30368 @2 Lower Hutt @3 NZL @Z 1 aut.`
A15	`01`			`@1 National Institute of Water and Atmospheric Research, Private Bag 14901 @2 Wellington 6041 @3 NZL @Z 1 aut.`
A15	`02`			`@1 School of Geography, Environment and Earth Sciences, Victoria University of Wellington, PO Box 600 @2 Wellington 6041 @3 NZL @Z 1 aut. @Z 3 aut. @Z 4 aut.`
A15	`03`			`@1 School of Environment, University of Auckland, Private Bag 92019 @2 Auckland 1142 @3 NZL @Z 2 aut.`
A20				`@1 75-81`
A21				`@1 2010`
A23	`01`			`@0 ENG`
A43	`01`			`@1 INIST @2 17236 @5 354000181715620060`
A44				`@0 0000 @1 © 2010 INIST-CNRS. All rights reserved.`
A45				`@0 3/4 p.`
A47	`01`	`1`		`@0 10-0252683`
A60				`@1 P`
A61				`@0 A`
A64	`01`	`1`		`@0 Journal of volcanology and geothermal research`
A66	`01`			`@0 GBR`
C01	`01`		`ENG`	@0 A crustal seismic reflection profile across the offshore Taupo Volcanic Zone (OTVZ) has been reprocessed to improve the lower crust-upper mantle image. The OTVZ is underlain by several strong sub-horizontal crustal reflections that may correspond to shear zones or mafic sills. A reflector interpreted to correspond to Moho lies at a depth of about 8-8.5 s twt (seconds two-way-traveltime) - about 20 km - under the western margin of the Raukumara Peninsula and rises to a depth of about 6 s twt (about 16 km) under the active, eastern part of the OTVZ and can be traced at about this depth across most of the OTVZ. Underlying this inferred Moho are two diffuse zones of discontinuous reflectivity, one underlying the active eastern OTVZ and a less well defined one underlying the landward extension of the Havre Trough. They extend from about 15 to 35 km depth, within the mantle wedge, and are inferred to be imaging a zone of depleted upper mantle associated with crustal extension. A localised zone of deep (30-50 km) reflectivity and seismicity occurs under the eastern OTVZ margin and may relate to fluid flow from the Hikurangi plateau being subducted further east.
C02	`01`	`2`		`@0 001E01F01`
C02	`02`	`2`		`@0 222A01`
C03	`01`	`2`	`FRE`	`@0 Sismique réflexion @5 01`
C03	`01`	`2`	`ENG`	`@0 seismic reflection @5 01`
C03	`01`	`2`	`SPA`	`@0 Método reflexión sísmica @5 01`
C03	`02`	`2`	`FRE`	`@0 Extension @5 02`
C03	`02`	`2`	`ENG`	`@0 extension @5 02`
C03	`02`	`2`	`SPA`	`@0 Extensión @5 02`
C03	`03`	`2`	`FRE`	`@0 Off shore @5 03`
C03	`03`	`2`	`ENG`	`@0 offshore @5 03`
C03	`03`	`2`	`SPA`	`@0 Off shore @5 03`
C03	`04`	`2`	`FRE`	`@0 Croûte terrestre inf @5 04`
C03	`04`	`2`	`ENG`	`@0 lower crust @5 04`
C03	`04`	`2`	`SPA`	`@0 Corteza terrestre inf @5 04`
C03	`05`	`2`	`FRE`	`@0 Manteau sup @5 05`
C03	`05`	`2`	`ENG`	`@0 upper mantle @5 05`
C03	`05`	`2`	`SPA`	`@0 Manto globo sup @5 05`
C03	`06`	`2`	`FRE`	`@0 Zone cisaillement @5 06`
C03	`06`	`2`	`ENG`	`@0 shear zones @5 06`
C03	`06`	`2`	`SPA`	`@0 Zona cizalla @5 06`
C03	`07`	`2`	`FRE`	`@0 Sill @5 07`
C03	`07`	`2`	`ENG`	`@0 sills @5 07`
C03	`07`	`2`	`SPA`	`@0 Sill @5 07`
C03	`08`	`2`	`FRE`	`@0 Réflecteur @5 08`
C03	`08`	`2`	`ENG`	`@0 reflectors @5 08`
C03	`09`	`2`	`FRE`	`@0 Profondeur @5 09`
C03	`09`	`2`	`ENG`	`@0 depth @5 09`
C03	`09`	`2`	`SPA`	`@0 Profundidad @5 09`
C03	`10`	`2`	`FRE`	`@0 Temps parcours @5 10`
C03	`10`	`2`	`ENG`	`@0 travel time @5 10`
C03	`10`	`2`	`SPA`	`@0 Tiempo recorrido @5 10`
C03	`11`	`2`	`FRE`	`@0 Fossé @5 11`
C03	`11`	`2`	`ENG`	`@0 troughs @5 11`
C03	`12`	`2`	`FRE`	`@0 Sismicité @5 12`
C03	`12`	`2`	`ENG`	`@0 seismicity @5 12`
C03	`12`	`2`	`SPA`	`@0 Sismicidad @5 12`
C03	`13`	`2`	`FRE`	`@0 Ecoulement @5 13`
C03	`13`	`2`	`ENG`	`@0 flow @5 13`
C03	`14`	`2`	`FRE`	`@0 Plateau @5 14`
C03	`14`	`2`	`ENG`	`@0 plateaus @5 14`
C03	`14`	`2`	`SPA`	`@0 Meseta @5 14`
C03	`15`	`2`	`FRE`	`@0 Croûte terrestre @5 15`
C03	`15`	`2`	`ENG`	`@0 crust @5 15`
C03	`15`	`2`	`SPA`	`@0 Corteza terrestre @5 15`
C03	`16`	`2`	`FRE`	`@0 Manteau appauvri @5 16`
C03	`16`	`2`	`ENG`	`@0 depleted mantle @5 16`
C03	`16`	`2`	`SPA`	`@0 Manto empobrecido @5 16`
C03	`17`	`2`	`FRE`	`@0 Zone volcanique Taupo @2 NG @5 61`
C03	`17`	`2`	`ENG`	`@0 Taupo volcanic zone @2 NG @5 61`
C03	`17`	`2`	`SPA`	`@0 Zona volcanica Taupo @2 NG @5 61`
C03	`18`	`2`	`FRE`	`@0 Péninsule Raukumara @2 NG @5 64`
C03	`18`	`2`	`ENG`	`@0 Raukumara Peninsula @2 NG @5 64`
C03	`18`	`2`	`SPA`	`@0 Península Raukumara @2 NG @5 64`
C07	`01`	`2`	`FRE`	`@0 Nouvelle Zélande Ile Nord @2 NG`
C07	`01`	`2`	`ENG`	`@0 North Island @2 NG`
C07	`01`	`2`	`SPA`	`@0 Nueva Zelanda Isla Norte @2 NG`
C07	`02`	`2`	`FRE`	`@0 Nouvelle Zélande @2 NG`
C07	`02`	`2`	`ENG`	`@0 New Zealand @2 NG`
C07	`02`	`2`	`SPA`	`@0 Nueva Zelandia @2 NG`
C07	`03`	`2`	`FRE`	`@0 Australasie`
C07	`03`	`2`	`ENG`	`@0 Australasia`
C07	`03`	`2`	`SPA`	`@0 Australasia`
N21				`@1 165`
N44	`01`			`@1 OTO`
N82				`@1 OTO`

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Pascal:10-0252683

Le document en format XML

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<sourceDesc><biblStruct><analytic><title xml:lang="en" level="a">Crustal seismic reflection measurements across the northern extension of the Taupo Volcanic Zone, North Island, New Zealand</title>
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<profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>Raukumara Peninsula</term>
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<keywords scheme="Pascal" xml:lang="fr"><term>Sismique réflexion</term>
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<front><div type="abstract" xml:lang="en">A crustal seismic reflection profile across the offshore Taupo Volcanic Zone (OTVZ) has been reprocessed to improve the lower crust-upper mantle image. The OTVZ is underlain by several strong sub-horizontal crustal reflections that may correspond to shear zones or mafic sills. A reflector interpreted to correspond to Moho lies at a depth of about 8-8.5 s twt (seconds two-way-traveltime) - about 20 km - under the western margin of the Raukumara Peninsula and rises to a depth of about 6 s twt (about 16 km) under the active, eastern part of the OTVZ and can be traced at about this depth across most of the OTVZ. Underlying this inferred Moho are two diffuse zones of discontinuous reflectivity, one underlying the active eastern OTVZ and a less well defined one underlying the landward extension of the Havre Trough. They extend from about 15 to 35 km depth, within the mantle wedge, and are inferred to be imaging a zone of depleted upper mantle associated with crustal extension. A localised zone of deep (30-50 km) reflectivity and seismicity occurs under the eastern OTVZ margin and may relate to fluid flow from the Hikurangi plateau being subducted further east.</div>
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<fC01 i1="01" l="ENG"><s0>A crustal seismic reflection profile across the offshore Taupo Volcanic Zone (OTVZ) has been reprocessed to improve the lower crust-upper mantle image. The OTVZ is underlain by several strong sub-horizontal crustal reflections that may correspond to shear zones or mafic sills. A reflector interpreted to correspond to Moho lies at a depth of about 8-8.5 s twt (seconds two-way-traveltime) - about 20 km - under the western margin of the Raukumara Peninsula and rises to a depth of about 6 s twt (about 16 km) under the active, eastern part of the OTVZ and can be traced at about this depth across most of the OTVZ. Underlying this inferred Moho are two diffuse zones of discontinuous reflectivity, one underlying the active eastern OTVZ and a less well defined one underlying the landward extension of the Havre Trough. They extend from about 15 to 35 km depth, within the mantle wedge, and are inferred to be imaging a zone of depleted upper mantle associated with crustal extension. A localised zone of deep (30-50 km) reflectivity and seismicity occurs under the eastern OTVZ margin and may relate to fluid flow from the Hikurangi plateau being subducted further east.</s0>
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<fC02 i1="02" i2="2"><s0>222A01</s0>
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<fC03 i1="01" i2="2" l="FRE"><s0>Sismique réflexion</s0>
<s5>01</s5>
</fC03>
<fC03 i1="01" i2="2" l="ENG"><s0>seismic reflection</s0>
<s5>01</s5>
</fC03>
<fC03 i1="01" i2="2" l="SPA"><s0>Método reflexión sísmica</s0>
<s5>01</s5>
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<fC03 i1="02" i2="2" l="FRE"><s0>Extension</s0>
<s5>02</s5>
</fC03>
<fC03 i1="02" i2="2" l="ENG"><s0>extension</s0>
<s5>02</s5>
</fC03>
<fC03 i1="02" i2="2" l="SPA"><s0>Extensión</s0>
<s5>02</s5>
</fC03>
<fC03 i1="03" i2="2" l="FRE"><s0>Off shore</s0>
<s5>03</s5>
</fC03>
<fC03 i1="03" i2="2" l="ENG"><s0>offshore</s0>
<s5>03</s5>
</fC03>
<fC03 i1="03" i2="2" l="SPA"><s0>Off shore</s0>
<s5>03</s5>
</fC03>
<fC03 i1="04" i2="2" l="FRE"><s0>Croûte terrestre inf</s0>
<s5>04</s5>
</fC03>
<fC03 i1="04" i2="2" l="ENG"><s0>lower crust</s0>
<s5>04</s5>
</fC03>
<fC03 i1="04" i2="2" l="SPA"><s0>Corteza terrestre inf</s0>
<s5>04</s5>
</fC03>
<fC03 i1="05" i2="2" l="FRE"><s0>Manteau sup</s0>
<s5>05</s5>
</fC03>
<fC03 i1="05" i2="2" l="ENG"><s0>upper mantle</s0>
<s5>05</s5>
</fC03>
<fC03 i1="05" i2="2" l="SPA"><s0>Manto globo sup</s0>
<s5>05</s5>
</fC03>
<fC03 i1="06" i2="2" l="FRE"><s0>Zone cisaillement</s0>
<s5>06</s5>
</fC03>
<fC03 i1="06" i2="2" l="ENG"><s0>shear zones</s0>
<s5>06</s5>
</fC03>
<fC03 i1="06" i2="2" l="SPA"><s0>Zona cizalla</s0>
<s5>06</s5>
</fC03>
<fC03 i1="07" i2="2" l="FRE"><s0>Sill</s0>
<s5>07</s5>
</fC03>
<fC03 i1="07" i2="2" l="ENG"><s0>sills</s0>
<s5>07</s5>
</fC03>
<fC03 i1="07" i2="2" l="SPA"><s0>Sill</s0>
<s5>07</s5>
</fC03>
<fC03 i1="08" i2="2" l="FRE"><s0>Réflecteur</s0>
<s5>08</s5>
</fC03>
<fC03 i1="08" i2="2" l="ENG"><s0>reflectors</s0>
<s5>08</s5>
</fC03>
<fC03 i1="09" i2="2" l="FRE"><s0>Profondeur</s0>
<s5>09</s5>
</fC03>
<fC03 i1="09" i2="2" l="ENG"><s0>depth</s0>
<s5>09</s5>
</fC03>
<fC03 i1="09" i2="2" l="SPA"><s0>Profundidad</s0>
<s5>09</s5>
</fC03>
<fC03 i1="10" i2="2" l="FRE"><s0>Temps parcours</s0>
<s5>10</s5>
</fC03>
<fC03 i1="10" i2="2" l="ENG"><s0>travel time</s0>
<s5>10</s5>
</fC03>
<fC03 i1="10" i2="2" l="SPA"><s0>Tiempo recorrido</s0>
<s5>10</s5>
</fC03>
<fC03 i1="11" i2="2" l="FRE"><s0>Fossé</s0>
<s5>11</s5>
</fC03>
<fC03 i1="11" i2="2" l="ENG"><s0>troughs</s0>
<s5>11</s5>
</fC03>
<fC03 i1="12" i2="2" l="FRE"><s0>Sismicité</s0>
<s5>12</s5>
</fC03>
<fC03 i1="12" i2="2" l="ENG"><s0>seismicity</s0>
<s5>12</s5>
</fC03>
<fC03 i1="12" i2="2" l="SPA"><s0>Sismicidad</s0>
<s5>12</s5>
</fC03>
<fC03 i1="13" i2="2" l="FRE"><s0>Ecoulement</s0>
<s5>13</s5>
</fC03>
<fC03 i1="13" i2="2" l="ENG"><s0>flow</s0>
<s5>13</s5>
</fC03>
<fC03 i1="14" i2="2" l="FRE"><s0>Plateau</s0>
<s5>14</s5>
</fC03>
<fC03 i1="14" i2="2" l="ENG"><s0>plateaus</s0>
<s5>14</s5>
</fC03>
<fC03 i1="14" i2="2" l="SPA"><s0>Meseta</s0>
<s5>14</s5>
</fC03>
<fC03 i1="15" i2="2" l="FRE"><s0>Croûte terrestre</s0>
<s5>15</s5>
</fC03>
<fC03 i1="15" i2="2" l="ENG"><s0>crust</s0>
<s5>15</s5>
</fC03>
<fC03 i1="15" i2="2" l="SPA"><s0>Corteza terrestre</s0>
<s5>15</s5>
</fC03>
<fC03 i1="16" i2="2" l="FRE"><s0>Manteau appauvri</s0>
<s5>16</s5>
</fC03>
<fC03 i1="16" i2="2" l="ENG"><s0>depleted mantle</s0>
<s5>16</s5>
</fC03>
<fC03 i1="16" i2="2" l="SPA"><s0>Manto empobrecido</s0>
<s5>16</s5>
</fC03>
<fC03 i1="17" i2="2" l="FRE"><s0>Zone volcanique Taupo</s0>
<s2>NG</s2>
<s5>61</s5>
</fC03>
<fC03 i1="17" i2="2" l="ENG"><s0>Taupo volcanic zone</s0>
<s2>NG</s2>
<s5>61</s5>
</fC03>
<fC03 i1="17" i2="2" l="SPA"><s0>Zona volcanica Taupo</s0>
<s2>NG</s2>
<s5>61</s5>
</fC03>
<fC03 i1="18" i2="2" l="FRE"><s0>Péninsule Raukumara</s0>
<s2>NG</s2>
<s5>64</s5>
</fC03>
<fC03 i1="18" i2="2" l="ENG"><s0>Raukumara Peninsula</s0>
<s2>NG</s2>
<s5>64</s5>
</fC03>
<fC03 i1="18" i2="2" l="SPA"><s0>Península Raukumara</s0>
<s2>NG</s2>
<s5>64</s5>
</fC03>
<fC07 i1="01" i2="2" l="FRE"><s0>Nouvelle Zélande Ile Nord</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="01" i2="2" l="ENG"><s0>North Island</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="01" i2="2" l="SPA"><s0>Nueva Zelanda Isla Norte</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="02" i2="2" l="FRE"><s0>Nouvelle Zélande</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="02" i2="2" l="ENG"><s0>New Zealand</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="02" i2="2" l="SPA"><s0>Nueva Zelandia</s0>
<s2>NG</s2>
</fC07>
<fC07 i1="03" i2="2" l="FRE"><s0>Australasie</s0>
</fC07>
<fC07 i1="03" i2="2" l="ENG"><s0>Australasia</s0>
</fC07>
<fC07 i1="03" i2="2" l="SPA"><s0>Australasia</s0>
</fC07>
<fN21><s1>165</s1>
</fN21>
<fN44 i1="01"><s1>OTO</s1>
</fN44>
<fN82><s1>OTO</s1>
</fN82>
</pA>
</standard>
</inist>
</record>

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   |texte=   Crustal seismic reflection measurements across the northern extension of the Taupo Volcanic Zone, North Island, New Zealand
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Crustal seismic reflection measurements across the northern extension of the Taupo Volcanic Zone, North Island, New Zealand

Crustal seismic reflection measurements across the northern extension of the Taupo Volcanic Zone, North Island, New Zealand

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