AustralieFrV1, PascalFrancis, Curation, bibRecord, 005763

Three-dimensional dynamic models of subducting plate-overriding plate-upper mantle interaction

Identifieur interne : 005763 ( PascalFrancis/Curation ); précédent : 005762; suivant : 005764

Three-dimensional dynamic models of subducting plate-overriding plate-upper mantle interaction

Auteurs : C. Meyer [France, Australie] ; W. P. Schellart [Australie]

Source :

Journal of geophysical research. Solid earth [ 2169-9313 ] ; 2013.

RBID : Pascal:13-0352947

Descripteurs français

Pascal (Inist)
- Modèle 3 dimensions, Dynamique, Plaque, Manteau sup, Subduction, Zone subduction, Interface, Epaisseur, Cinématique, Déformation, Dalle, Discontinuité, Pendage, Fosse abyssale, Mouvement, Extension, Succion, Cisaillement, Ecoulement, Coulée, Contrainte, Flottabilité, Corrélation.

English descriptors

KwdEn :
- buoyancy, correlation, deformation, dip, discontinuities, dynamics, extension, flow, flows, interfaces, kinematics, movement, plates, shear, slabs, stress, subduction, subduction zones, suction, thickness, three-dimensional models, trenches, upper mantle.

Abstract

[1] We present fully dynamic generic three-dimensional laboratory models of progressive subduction with an overriding plate and a weak subduction zone interface. Overriding plate thickness (T_OP) is varied systematically (in the range 0-2.5 cm scaling to 0-125 km) to investigate its effect on subduction kinematics and overriding plate deformation. The general pattern of subduction is the same for all models with slab draping on the 670 km discontinuity, comparable slab dip angles, trench retreat, trenchward subducting plate motion, and a concave trench curvature. The narrow slab models only show overriding plate extension. Subduction partitioning (ν_SP⊥/(ν_SP⊥+ν_T⊥)) increases with increasing Top, where trenchward subducting plate motion (ν_SP⊥) increases at the expense of trench retreat (ν_T⊥). This results from an increase in trench suction force with increasing T_OP, which retards trench retreat. An increase in T_OP also corresponds to a decrease in overriding plate extension and curvature because a thicker overriding plate provides more resistance to deform. Overriding plate extension is maximum at a scaled distance of ∼200-400 km from the trench, not at the trench, suggesting that basal shear tractions resulting from mantle flow below the overriding plate primarily drive extension rather than deviatoric tensional normal stresses at the subduction zone interface. The force that drives overriding plate extension is 5%-11% of the slab negative buoyancy force. The models show a positive correlation between ν_T⊥ and overriding plate extension rate, in agreement with observations. The results suggest that slab rollback and associated toroidal mantle flow drive overriding plate extension and backarc basin formation.

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A08	`01`	`1`	`ENG`	`@1 Three-dimensional dynamic models of subducting plate-overriding plate-upper mantle interaction`
A11	`01`	`1`		`@1 MEYER (C.)`
A11	`02`	`1`		`@1 SCHELLART (W. P.)`
A14	`01`			`@1 Ecole Normale Supérieure @2 Paris @3 FRA @Z 1 aut.`
A14	`02`			`@1 School of Geosciences, Monash University @2 Melbourne, Victoria @3 AUS @Z 1 aut. @Z 2 aut.`
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C01	`01`		`ENG`	@0 [1] We present fully dynamic generic three-dimensional laboratory models of progressive subduction with an overriding plate and a weak subduction zone interface. Overriding plate thickness (T_OP) is varied systematically (in the range 0-2.5 cm scaling to 0-125 km) to investigate its effect on subduction kinematics and overriding plate deformation. The general pattern of subduction is the same for all models with slab draping on the 670 km discontinuity, comparable slab dip angles, trench retreat, trenchward subducting plate motion, and a concave trench curvature. The narrow slab models only show overriding plate extension. Subduction partitioning (ν_SP⊥/(ν_SP⊥+ν_T⊥)) increases with increasing Top, where trenchward subducting plate motion (ν_SP⊥) increases at the expense of trench retreat (ν_T⊥). This results from an increase in trench suction force with increasing T_OP, which retards trench retreat. An increase in T_OP also corresponds to a decrease in overriding plate extension and curvature because a thicker overriding plate provides more resistance to deform. Overriding plate extension is maximum at a scaled distance of ∼200-400 km from the trench, not at the trench, suggesting that basal shear tractions resulting from mantle flow below the overriding plate primarily drive extension rather than deviatoric tensional normal stresses at the subduction zone interface. The force that drives overriding plate extension is 5%-11% of the slab negative buoyancy force. The models show a positive correlation between ν_T⊥ and overriding plate extension rate, in agreement with observations. The results suggest that slab rollback and associated toroidal mantle flow drive overriding plate extension and backarc basin formation.
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C03	`03`	`2`	`SPA`	`@0 Placa @5 03`
C03	`04`	`2`	`FRE`	`@0 Manteau sup @5 04`
C03	`04`	`2`	`ENG`	`@0 upper mantle @5 04`
C03	`04`	`2`	`SPA`	`@0 Manto globo sup @5 04`
C03	`05`	`2`	`FRE`	`@0 Subduction @5 05`
C03	`05`	`2`	`ENG`	`@0 subduction @5 05`
C03	`05`	`2`	`SPA`	`@0 Subducción @5 05`
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C03	`06`	`2`	`ENG`	`@0 subduction zones @5 06`
C03	`06`	`2`	`SPA`	`@0 Zona subducto @5 06`
C03	`07`	`2`	`FRE`	`@0 Interface @5 07`
C03	`07`	`2`	`ENG`	`@0 interfaces @5 07`
C03	`07`	`2`	`SPA`	`@0 Interfase @5 07`
C03	`08`	`2`	`FRE`	`@0 Epaisseur @5 08`
C03	`08`	`2`	`ENG`	`@0 thickness @5 08`
C03	`08`	`2`	`SPA`	`@0 Espesor @5 08`
C03	`09`	`2`	`FRE`	`@0 Cinématique @5 10`
C03	`09`	`2`	`ENG`	`@0 kinematics @5 10`
C03	`09`	`2`	`SPA`	`@0 Cinemática @5 10`
C03	`10`	`2`	`FRE`	`@0 Déformation @5 11`
C03	`10`	`2`	`ENG`	`@0 deformation @5 11`
C03	`11`	`2`	`FRE`	`@0 Dalle @5 12`
C03	`11`	`2`	`ENG`	`@0 slabs @5 12`
C03	`11`	`2`	`SPA`	`@0 Losa @5 12`
C03	`12`	`2`	`FRE`	`@0 Discontinuité @5 13`
C03	`12`	`2`	`ENG`	`@0 discontinuities @5 13`
C03	`12`	`2`	`SPA`	`@0 Discontinuidad @5 13`
C03	`13`	`2`	`FRE`	`@0 Pendage @5 14`
C03	`13`	`2`	`ENG`	`@0 dip @5 14`
C03	`13`	`2`	`SPA`	`@0 Buzamiento @5 14`
C03	`14`	`2`	`FRE`	`@0 Fosse abyssale @5 15`
C03	`14`	`2`	`ENG`	`@0 trenches @5 15`
C03	`14`	`2`	`SPA`	`@0 Fosa abisal @5 15`
C03	`15`	`2`	`FRE`	`@0 Mouvement @5 16`
C03	`15`	`2`	`ENG`	`@0 movement @5 16`
C03	`16`	`2`	`FRE`	`@0 Extension @5 17`
C03	`16`	`2`	`ENG`	`@0 extension @5 17`
C03	`16`	`2`	`SPA`	`@0 Extensión @5 17`
C03	`17`	`2`	`FRE`	`@0 Succion @5 18`
C03	`17`	`2`	`ENG`	`@0 suction @5 18`
C03	`17`	`2`	`SPA`	`@0 Succión @5 18`
C03	`18`	`2`	`FRE`	`@0 Cisaillement @5 19`
C03	`18`	`2`	`ENG`	`@0 shear @5 19`
C03	`18`	`2`	`SPA`	`@0 Cizalladura @5 19`
C03	`19`	`2`	`FRE`	`@0 Ecoulement @5 20`
C03	`19`	`2`	`ENG`	`@0 flow @5 20`
C03	`20`	`2`	`FRE`	`@0 Coulée @5 21`
C03	`20`	`2`	`ENG`	`@0 flows @5 21`
C03	`20`	`2`	`SPA`	`@0 Colada @5 21`
C03	`21`	`2`	`FRE`	`@0 Contrainte @5 22`
C03	`21`	`2`	`ENG`	`@0 stress @5 22`
C03	`21`	`2`	`SPA`	`@0 Coacción @5 22`
C03	`22`	`2`	`FRE`	`@0 Flottabilité @5 23`
C03	`22`	`2`	`ENG`	`@0 buoyancy @5 23`
C03	`22`	`2`	`SPA`	`@0 Flotabilidad @5 23`
C03	`23`	`2`	`FRE`	`@0 Corrélation @5 24`
C03	`23`	`2`	`ENG`	`@0 correlation @5 24`
C03	`23`	`2`	`SPA`	`@0 Correlación @5 24`
N21				`@1 336`

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Le document en format XML

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<profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>buoyancy</term>
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<term>slabs</term>
<term>stress</term>
<term>subduction</term>
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<term>suction</term>
<term>thickness</term>
<term>three-dimensional models</term>
<term>trenches</term>
<term>upper mantle</term>
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<keywords scheme="Pascal" xml:lang="fr"><term>Modèle 3 dimensions</term>
<term>Dynamique</term>
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<term>Interface</term>
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<front><div type="abstract" xml:lang="en">[1] We present fully dynamic generic three-dimensional laboratory models of progressive subduction with an overriding plate and a weak subduction zone interface. Overriding plate thickness (T<sub>OP</sub>
) is varied systematically (in the range 0-2.5 cm scaling to 0-125 km) to investigate its effect on subduction kinematics and overriding plate deformation. The general pattern of subduction is the same for all models with slab draping on the 670 km discontinuity, comparable slab dip angles, trench retreat, trenchward subducting plate motion, and a concave trench curvature. The narrow slab models only show overriding plate extension. Subduction partitioning (ν<sub>SP</sub>
⊥/(ν<sub>SP</sub>
⊥+ν<sub>T</sub>
⊥)) increases with increasing Top, where trenchward subducting plate motion (ν<sub>SP</sub>
⊥) increases at the expense of trench retreat (ν<sub>T</sub>
⊥). This results from an increase in trench suction force with increasing T<sub>OP</sub>
, which retards trench retreat. An increase in T<sub>OP</sub>
 also corresponds to a decrease in overriding plate extension and curvature because a thicker overriding plate provides more resistance to deform. Overriding plate extension is maximum at a scaled distance of ∼200-400 km from the trench, not at the trench, suggesting that basal shear tractions resulting from mantle flow below the overriding plate primarily drive extension rather than deviatoric tensional normal stresses at the subduction zone interface. The force that drives overriding plate extension is 5%-11% of the slab negative buoyancy force. The models show a positive correlation between ν<sub>T</sub>
⊥ and overriding plate extension rate, in agreement with observations. The results suggest that slab rollback and associated toroidal mantle flow drive overriding plate extension and backarc basin formation.</div>
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<fC01 i1="01" l="ENG"><s0>[1] We present fully dynamic generic three-dimensional laboratory models of progressive subduction with an overriding plate and a weak subduction zone interface. Overriding plate thickness (T<sub>OP</sub>
) is varied systematically (in the range 0-2.5 cm scaling to 0-125 km) to investigate its effect on subduction kinematics and overriding plate deformation. The general pattern of subduction is the same for all models with slab draping on the 670 km discontinuity, comparable slab dip angles, trench retreat, trenchward subducting plate motion, and a concave trench curvature. The narrow slab models only show overriding plate extension. Subduction partitioning (ν<sub>SP</sub>
⊥/(ν<sub>SP</sub>
⊥+ν<sub>T</sub>
⊥)) increases with increasing Top, where trenchward subducting plate motion (ν<sub>SP</sub>
⊥) increases at the expense of trench retreat (ν<sub>T</sub>
⊥). This results from an increase in trench suction force with increasing T<sub>OP</sub>
, which retards trench retreat. An increase in T<sub>OP</sub>
 also corresponds to a decrease in overriding plate extension and curvature because a thicker overriding plate provides more resistance to deform. Overriding plate extension is maximum at a scaled distance of ∼200-400 km from the trench, not at the trench, suggesting that basal shear tractions resulting from mantle flow below the overriding plate primarily drive extension rather than deviatoric tensional normal stresses at the subduction zone interface. The force that drives overriding plate extension is 5%-11% of the slab negative buoyancy force. The models show a positive correlation between ν<sub>T</sub>
⊥ and overriding plate extension rate, in agreement with observations. The results suggest that slab rollback and associated toroidal mantle flow drive overriding plate extension and backarc basin formation.</s0>
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<fC03 i1="03" i2="2" l="FRE"><s0>Plaque</s0>
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<fC03 i1="03" i2="2" l="ENG"><s0>plates</s0>
<s5>03</s5>
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<fC03 i1="03" i2="2" l="SPA"><s0>Placa</s0>
<s5>03</s5>
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<fC03 i1="04" i2="2" l="FRE"><s0>Manteau sup</s0>
<s5>04</s5>
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<fC03 i1="04" i2="2" l="ENG"><s0>upper mantle</s0>
<s5>04</s5>
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<fC03 i1="04" i2="2" l="SPA"><s0>Manto globo sup</s0>
<s5>04</s5>
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<fC03 i1="05" i2="2" l="FRE"><s0>Subduction</s0>
<s5>05</s5>
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<fC03 i1="05" i2="2" l="ENG"><s0>subduction</s0>
<s5>05</s5>
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<fC03 i1="05" i2="2" l="SPA"><s0>Subducción</s0>
<s5>05</s5>
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<fC03 i1="06" i2="2" l="FRE"><s0>Zone subduction</s0>
<s5>06</s5>
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<fC03 i1="06" i2="2" l="ENG"><s0>subduction zones</s0>
<s5>06</s5>
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<fC03 i1="06" i2="2" l="SPA"><s0>Zona subducto</s0>
<s5>06</s5>
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<fC03 i1="07" i2="2" l="FRE"><s0>Interface</s0>
<s5>07</s5>
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<fC03 i1="07" i2="2" l="ENG"><s0>interfaces</s0>
<s5>07</s5>
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<fC03 i1="07" i2="2" l="SPA"><s0>Interfase</s0>
<s5>07</s5>
</fC03>
<fC03 i1="08" i2="2" l="FRE"><s0>Epaisseur</s0>
<s5>08</s5>
</fC03>
<fC03 i1="08" i2="2" l="ENG"><s0>thickness</s0>
<s5>08</s5>
</fC03>
<fC03 i1="08" i2="2" l="SPA"><s0>Espesor</s0>
<s5>08</s5>
</fC03>
<fC03 i1="09" i2="2" l="FRE"><s0>Cinématique</s0>
<s5>10</s5>
</fC03>
<fC03 i1="09" i2="2" l="ENG"><s0>kinematics</s0>
<s5>10</s5>
</fC03>
<fC03 i1="09" i2="2" l="SPA"><s0>Cinemática</s0>
<s5>10</s5>
</fC03>
<fC03 i1="10" i2="2" l="FRE"><s0>Déformation</s0>
<s5>11</s5>
</fC03>
<fC03 i1="10" i2="2" l="ENG"><s0>deformation</s0>
<s5>11</s5>
</fC03>
<fC03 i1="11" i2="2" l="FRE"><s0>Dalle</s0>
<s5>12</s5>
</fC03>
<fC03 i1="11" i2="2" l="ENG"><s0>slabs</s0>
<s5>12</s5>
</fC03>
<fC03 i1="11" i2="2" l="SPA"><s0>Losa</s0>
<s5>12</s5>
</fC03>
<fC03 i1="12" i2="2" l="FRE"><s0>Discontinuité</s0>
<s5>13</s5>
</fC03>
<fC03 i1="12" i2="2" l="ENG"><s0>discontinuities</s0>
<s5>13</s5>
</fC03>
<fC03 i1="12" i2="2" l="SPA"><s0>Discontinuidad</s0>
<s5>13</s5>
</fC03>
<fC03 i1="13" i2="2" l="FRE"><s0>Pendage</s0>
<s5>14</s5>
</fC03>
<fC03 i1="13" i2="2" l="ENG"><s0>dip</s0>
<s5>14</s5>
</fC03>
<fC03 i1="13" i2="2" l="SPA"><s0>Buzamiento</s0>
<s5>14</s5>
</fC03>
<fC03 i1="14" i2="2" l="FRE"><s0>Fosse abyssale</s0>
<s5>15</s5>
</fC03>
<fC03 i1="14" i2="2" l="ENG"><s0>trenches</s0>
<s5>15</s5>
</fC03>
<fC03 i1="14" i2="2" l="SPA"><s0>Fosa abisal</s0>
<s5>15</s5>
</fC03>
<fC03 i1="15" i2="2" l="FRE"><s0>Mouvement</s0>
<s5>16</s5>
</fC03>
<fC03 i1="15" i2="2" l="ENG"><s0>movement</s0>
<s5>16</s5>
</fC03>
<fC03 i1="16" i2="2" l="FRE"><s0>Extension</s0>
<s5>17</s5>
</fC03>
<fC03 i1="16" i2="2" l="ENG"><s0>extension</s0>
<s5>17</s5>
</fC03>
<fC03 i1="16" i2="2" l="SPA"><s0>Extensión</s0>
<s5>17</s5>
</fC03>
<fC03 i1="17" i2="2" l="FRE"><s0>Succion</s0>
<s5>18</s5>
</fC03>
<fC03 i1="17" i2="2" l="ENG"><s0>suction</s0>
<s5>18</s5>
</fC03>
<fC03 i1="17" i2="2" l="SPA"><s0>Succión</s0>
<s5>18</s5>
</fC03>
<fC03 i1="18" i2="2" l="FRE"><s0>Cisaillement</s0>
<s5>19</s5>
</fC03>
<fC03 i1="18" i2="2" l="ENG"><s0>shear</s0>
<s5>19</s5>
</fC03>
<fC03 i1="18" i2="2" l="SPA"><s0>Cizalladura</s0>
<s5>19</s5>
</fC03>
<fC03 i1="19" i2="2" l="FRE"><s0>Ecoulement</s0>
<s5>20</s5>
</fC03>
<fC03 i1="19" i2="2" l="ENG"><s0>flow</s0>
<s5>20</s5>
</fC03>
<fC03 i1="20" i2="2" l="FRE"><s0>Coulée</s0>
<s5>21</s5>
</fC03>
<fC03 i1="20" i2="2" l="ENG"><s0>flows</s0>
<s5>21</s5>
</fC03>
<fC03 i1="20" i2="2" l="SPA"><s0>Colada</s0>
<s5>21</s5>
</fC03>
<fC03 i1="21" i2="2" l="FRE"><s0>Contrainte</s0>
<s5>22</s5>
</fC03>
<fC03 i1="21" i2="2" l="ENG"><s0>stress</s0>
<s5>22</s5>
</fC03>
<fC03 i1="21" i2="2" l="SPA"><s0>Coacción</s0>
<s5>22</s5>
</fC03>
<fC03 i1="22" i2="2" l="FRE"><s0>Flottabilité</s0>
<s5>23</s5>
</fC03>
<fC03 i1="22" i2="2" l="ENG"><s0>buoyancy</s0>
<s5>23</s5>
</fC03>
<fC03 i1="22" i2="2" l="SPA"><s0>Flotabilidad</s0>
<s5>23</s5>
</fC03>
<fC03 i1="23" i2="2" l="FRE"><s0>Corrélation</s0>
<s5>24</s5>
</fC03>
<fC03 i1="23" i2="2" l="ENG"><s0>correlation</s0>
<s5>24</s5>
</fC03>
<fC03 i1="23" i2="2" l="SPA"><s0>Correlación</s0>
<s5>24</s5>
</fC03>
<fN21><s1>336</s1>
</fN21>
</pA>
</standard>
</inist>
</record>

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   |texte=   Three-dimensional dynamic models of subducting plate-overriding plate-upper mantle interaction
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	Serveur d'exploration sur les relations entre la France et l'Australie
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Serveur d'exploration sur les relations entre la France et l'Australie

Three-dimensional dynamic models of subducting plate-overriding plate-upper mantle interaction

Three-dimensional dynamic models of subducting plate-overriding plate-upper mantle interaction

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