Tectonics and geothermal Tectonics and geothermal exploration and - - PowerPoint PPT Presentation

tectonics and geothermal tectonics and geothermal
SMART_READER_LITE
LIVE PREVIEW

Tectonics and geothermal Tectonics and geothermal exploration and - - PowerPoint PPT Presentation

Tectonics and geothermal Tectonics and geothermal exploration and production exploration and production Sierd Cloetingh, Jan-Diederik van Wees, Fred Sierd Cloetingh, Jan-Diederik van Wees, Fred Beekman, Magdala Tesauro, Nico Hardenbol,


slide-1
SLIDE 1

Tectonics and geothermal exploration and production Tectonics and geothermal exploration and production

Sierd Cloetingh, Jan-Diederik van Wees, Fred Beekman, Magdala Tesauro, Nico Hardenbol, Marlies ter Voorde Sierd Cloetingh, Jan-Diederik van Wees, Fred Beekman, Magdala Tesauro, Nico Hardenbol, Marlies ter Voorde

ENGINE mid term meeting ENGINE mid term meeting

12 12 Januari Januari 2007 2007

ISES

Netherlands Research Centre for Integrated Solid Earth Science

vrije Universiteit amsterdam

slide-2
SLIDE 2

Spakman (2006) Artemieva et al. (2006)

Europe: heterogeneous crustal and mantle structure Europe: heterogeneous crustal and mantle structure

slide-3
SLIDE 3

mantle lithosphere astenosphere astenosphere lower crust Moho crust upper sed

  • 3D geometrical &

compositional model from digital elevation models, seismic data, gravity, and ENTEC/EUCOR-URGENT/GFZ databases

  • Calculations using a mix of

in-house developed and commercial software

  • Access to LOFAR’s “Blue

Gene” grid computing network

  • Model resolution will increase

iteratively during the project

  • Grid cells may have a

different size

  • Final size of the grid cells will

depend on the quality of the (geological) input data

STEP 1: 3D geometry & composition STEP 2: 3D temperature STEP 3: 3D strength STEP 4: 3D stress & strain

Cloetingh et al., 2005, QSR

3D models of strength, stress and strain of the European continental lithosphere 3D models of strength, stress and strain of the European continental lithosphere

slide-4
SLIDE 4

Construction of the rheological strength maps Construction of the rheological strength maps

Hardebol et al., 2006

slide-5
SLIDE 5

Maps of the integrated strength distribution of the European lithosphere will allow to identify zones of intense localized deformation and high risk seismic zones

  • Distributed versus localized

deformation

  • Strong eastern European

craton versus weak western European lithosphere

  • Weak rifts and basins

versus strong indentors

Cloetingh et al., 2005, QSR

Integrated strength maps of the European lithosphere Integrated strength maps of the European lithosphere

slide-6
SLIDE 6

Regional component of residual gravity mantle anomaly Regional component of residual gravity mantle anomaly

Tesauro et al., 2007

slide-7
SLIDE 7

Cloetingh et al., 2006, ESR

Correlation between seismicity and crustal strength Correlation between seismicity and crustal strength

slide-8
SLIDE 8

Innovative Modeling of Mantle-to-Lithosphere-to-Surface Processes Innovative Modeling of Mantle-to-Lithosphere-to-Surface Processes

Burov, 2007, GPC Burov and Cloetingh, 1997, EPSL

slide-9
SLIDE 9

Linking the sedimentary record to the underlying lithosphere Linking the sedimentary record to the underlying lithosphere

Japsen, 2007

slide-10
SLIDE 10

Ritter et al., 2001

Tomographic sections across the Eifel plume Tomographic sections across the Eifel plume

slide-11
SLIDE 11

Coupling between deep Earth and surface processes Coupling between deep Earth and surface processes

Guillou-Frottier et al., 2007

slide-12
SLIDE 12

Guillou-Frottier et al., 2007

Coupling between mantle and surface processes Coupling between mantle and surface processes

slide-13
SLIDE 13

Type-2 model simulating the collision between two different lithospheric blocks Type-1 model representing a cold lithosphere with a strong upper mantle Sokoutis et al., 2005. Tectonophysics

Analogue modelling of intraplate deformation

slide-14
SLIDE 14

ESF EUROCORES TOPO-EUROPE ESF EUROCORES TOPO-EUROPE

The Natural Laboratory Concept on coupled deep Earth – surface processes The Natural Laboratory Concept on coupled deep Earth – surface processes

slide-15
SLIDE 15

Within the orogen: the Alps/Carpathians–Pannonian Basin System Within the orogen: the Alps/Carpathians–Pannonian Basin System

Grenerczy et al. 2005

Vrancea Vrancea

Nubia Nubia

Extension at Extension at Appennines Appennines

Effect of the Effect of the Aegean Aegean

Velocity scale mm/yr Velocity scale mm/yr 4 4

Surface velocity map

slide-16
SLIDE 16

Basin formation and evolution in a back-arc setting Basin formation and evolution in a back-arc setting

Horvath et al. 2006

slide-17
SLIDE 17

Stress distribution transect across the Pannonian basin Stress distribution transect across the Pannonian basin

Bada et al. 2007

slide-18
SLIDE 18

Seismic tomography Seismic tomography

Martin et al. 2006

slide-19
SLIDE 19

TOPO-EUROPE: From Source to Sink TOPO-EUROPE: From Source to Sink

slide-20
SLIDE 20

Alpine tectonics and present thermal structure

Willingshofer and Cloetingh, Tectonics 22, 2003

slide-21
SLIDE 21

Pyrenean or ‘Iberian’ phase Paleogene- Early Neogene N-S to NE-SW compression Valencian phase E.Miocene - Pliocene WNW-ESE extension Betic phase NNW-SSE compression

  • M. Miocene-recent

Ridge Push from the Atlantic (M. -L. Cretaceous till present day)

Significant intraplate deformation Vertical motions Erosion/sedimentation/tectonics INTRAPLATE RECORD OF STRESS FIELD (CHANGES): Tertiary basin formation and deformation Polyphase fault reactivation under different stress fields

Cloetingh et al., 2002, Tectonics

Intraplate deformation in micro-continent Iberia

slide-22
SLIDE 22

Catalan Coastal Range

37-35 Ma

Garcia-Castellanos et al., 2003. JGR

Ebro Basin: From a typical foreland basin to a closed drainage system

Pyrenees Iberian R. CCR

Valencia

Trough

slide-23
SLIDE 23

Catalan Coastal Range Granites marked by recent Erosion related to

  • pening of Valencia Trough

Larre and Andriessen, 2006

slide-24
SLIDE 24

Catalan Coastal Ranges: numerical modelling of effect of recent erosion on heat flow in granites

Ter Voorde et al., EPSL, 2004

Normal Geotherm Elevated Geotherm Due to erosion

slide-25
SLIDE 25

Conclusions and Perspectives Conclusions and Perspectives

  • Tectonic modelling provides key constraints on crustal stress and

temperature, helpful for geothermal exploration beyond well control

  • Late Tertiary tectonics have strong influence on spatial variation
  • f crustal heat flow and stress
  • Interplay of lithospheric and surface processes operating at

multiple scales need to be taken into account for understanding and prediction of crustal stress and heat flow

  • Analogue-numerical modelling applied in natural laboratories

provide a set of world class opportunities to develop a new generation of models for crustal stress and heat flow evolution