lithosphere extension in 3-d (oblique rifting, rift propagation) jolante van wijk & donna...
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Lithosphere extension in 3-DLithosphere extension in 3-D(oblique rifting, rift propagation)(oblique rifting, rift propagation)
Jolante van WijkJolante van Wijk
&&
Donna BlackmanDonna Blackman
SIOSIO
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Lithosphere extension: 2-D or 3-DLithosphere extension: 2-D or 3-D
Jan Mayen Fracture ZoneJan Mayen Fracture Zone
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OutlineOutline
* 3-D cases and tectonic processes involved* 3-D cases and tectonic processes involved-oblique rifting-oblique rifting-rift propagation-rift propagation-mantle flow beneath -mantle flow beneath rifts rifts
* Prior modeling approaches* Prior modeling approaches -numerical-numerical-analogue-analogue
* Our approach: Tekton & FELIB* Our approach: Tekton & FELIB
* Other options* Other options
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Woodlark BasinWoodlark Basin
Rift propagationRift propagation
Lithosphere extension: 3-D processesLithosphere extension: 3-D processes
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Gulf of AdenGulf of Aden
Lithosphere extension: 3-D processesLithosphere extension: 3-D processes
Rift propagationRift propagation
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Caledonian-Caledonian-HercynianHercynianbeltsbelts
NAGFNAGF
Lithosphere extension: 3-D processesLithosphere extension: 3-D processes
Pre-structured lithosphere, oblique riftingPre-structured lithosphere, oblique rifting
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Lithosphere extension: 3-D processesLithosphere extension: 3-D processes
EARS follows pre-structured lithosphereEARS follows pre-structured lithosphere
Ebinger, 2005Ebinger, 2005
Extension of continental Extension of continental lithospherelithosphere
MechanicalMechanicalstretchingstretching
MagmaticMagmaticextensionextension
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Lithosphere extension: 3-D processesLithosphere extension: 3-D processes
Rift branches Proterozoic mobile beltsRift branches Proterozoic mobile belts
MadagascarMadagascar
AfricaAfrica
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Lithosphere extension: 2-D processesLithosphere extension: 2-D processes
Decompressional melting during extensionDecompressional melting during extension
Ebinger, 2005Ebinger, 2005
Extension of continental Extension of continental lithospherelithosphere
MechanicalMechanicalstretchingstretching
MagmaticMagmaticextensionextension
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Lithosphere extension: 3-D processesLithosphere extension: 3-D processes
Tectonic processes involvedTectonic processes involved
Setup geometry Setup geometry lateral variations in lithosphere lateral variations in lithosphere architecture, different geological architecture, different geological provincesprovinces
Boundary conditionsBoundary conditions laterally varying boundary conditions,laterally varying boundary conditions,oblique extensionoblique extension
Basics needs:Basics needs:
Thermo-mechanical model?Thermo-mechanical model?Layered lithosphere?Layered lithosphere?
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Existing numerical modelsExisting numerical models
Elastic Plate Model: Elastic Plate Model: Hubert-Ferrari et al., 2003Hubert-Ferrari et al., 2003
Rift propagation (=crack propagation)Rift propagation (=crack propagation)
Assumption: lithosphere is an elasticAssumption: lithosphere is an elasticplate in which viscous/ductile behaviorplate in which viscous/ductile behaviorplays no (important) roleplays no (important) role
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Existing numerical modelsExisting numerical models
Finite Element Models:Finite Element Models: Dunbar and Sawyer, 1996 Dunbar and Sawyer, 1996
Rift propagationRift propagation
- Symmetrical model- Symmetrical model- Equations: creeping flow, heat flow- Equations: creeping flow, heat flow
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Existing numerical modelsExisting numerical models
Boundary Element Models: Boundary Element Models: Katzman, ten Brink & Lin, 1995Katzman, ten Brink & Lin, 1995
Pull-apart basin formationPull-apart basin formation
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Analogue modeling studiesAnalogue modeling studies
(Tron and Brun, 1991)(Tron and Brun, 1991)
Sand & silicone experimentsSand & silicone experiments
+ fault structures+ fault structures - thermal effects, rheology- thermal effects, rheology
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More analogue results
Analogue modeling studies of oblique riftingAnalogue modeling studies of oblique rifting
(Giacomo Corti, 2004)(Giacomo Corti, 2004)
Centrifuge modelCentrifuge model
+ fault structures+ fault structures - thermal effects, rheology- thermal effects, rheology
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Our modeling approachOur modeling approach
Finite element model, Lagrangian approachFinite element model, Lagrangian approach
Mechanical part: based on TektonMechanical part: based on Tekton
Thermal part: based on FELIBThermal part: based on FELIB
Thermo-mechanical modelThermo-mechanical model
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Numerical modeling of oblique riftingNumerical modeling of oblique rifting
Mechanical part Mechanical part Thermal partThermal part
Visco-elastic deformation,Visco-elastic deformation, Heat flow equationHeat flow equationcorrection for plastic/brittlecorrection for plastic/brittle Heat production in crustHeat production in crustbehaviorbehavior
Buoyancy forcesBuoyancy forces
T-dependent power-T-dependent power-law rheologylaw rheology
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Numerical modeling of oblique riftingNumerical modeling of oblique rifting
Model setupModel setup
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Oblique riftingOblique rifting
Results: Map view of model domain, crustal thinningResults: Map view of model domain, crustal thinning
ObliqueOblique riftingrifting
ObliqueOblique riftingrifting
NormalNormal riftingrifting
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Oblique riftingOblique rifting
Results: Surface heat flow for oblique rifting testResults: Surface heat flow for oblique rifting test
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* Rift zones follow the weak trend as a group, but are* Rift zones follow the weak trend as a group, but are individually oriented according to extension directionindividually oriented according to extension direction
* Asymmetric development of individual rifts* Asymmetric development of individual rifts
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* Rift zones follow the weak trend as a group, but are* Rift zones follow the weak trend as a group, but are individually oriented according to extension directionindividually oriented according to extension direction
* Asymmetric development of individual rifts* Asymmetric development of individual rifts
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*Asymmetric development of individual rifts*Asymmetric development of individual rifts
*Alternating asymmetric rifts, linked through *Alternating asymmetric rifts, linked through accommodation zones accommodation zones
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Example of alternating rift asymmetry can beExample of alternating rift asymmetry can befound in the Malawi Riftfound in the Malawi Rift
Lake MalawiLake Malawi topographytopography
Ebinger et al., 1987Ebinger et al., 1987
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Mantle flow beneath rift basinMantle flow beneath rift basin
Rift parallelRift parallel
Rift perpendicularRift perpendicular
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Rift propagation modelingRift propagation modeling
Model setupModel setup
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Rift propagation: end-member modesRift propagation: end-member modes
Evolution of crustal thinning, map view of model domainEvolution of crustal thinning, map view of model domain
StrongStrongplateplate
WeakWeakplateplate
Inter-Inter-mediatemediate
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Rift propagation: end-member modesRift propagation: end-member modes
Rift-parallel component of velocity field, map viewRift-parallel component of velocity field, map view
Stalled riftStalled rift
Continuous Continuous propagationpropagation
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Rift propagation: end-member modesRift propagation: end-member modes
Horizontal shear stress, map viewHorizontal shear stress, map view
Stalled riftStalled rift
Continuous Continuous propagationpropagation
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* Modeling of smaller scale structures * Modeling of smaller scale structures
* Grid spacing, calculation time* Grid spacing, calculation time
* Remeshing, large deformation* Remeshing, large deformation
* Brittle/ductile behavior* Brittle/ductile behavior
Improvements neededImprovements needed
What works fineWhat works fine
* Flexibility of geometry, initial setup and boundary conditions* Flexibility of geometry, initial setup and boundary conditions
* Application to deformation of oceanic lithosphere* Application to deformation of oceanic lithosphere
* Modeling of large scale structures* Modeling of large scale structures
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SNAC?SNAC?
Commercial codes such asCommercial codes such as ANSYSANSYSABAQUSABAQUS……....FLACFLAC
Other optionsOther options
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