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Tectonics of Venus

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Subduction to flood basalts to hot spot volcanism (Herrick 1992, also Basilevsky ... Subduction to Hot Spot Model. Prior to 800 Ma active subduction and plate ... – PowerPoint PPT presentation

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Title: Tectonics of Venus


1
Tectonics of Venus
2
Earths Sister Planet
  • Similarities
  • Terrestrial
  • Size
  • Density
  • Relative distance to the Sun
  • Relatively young surfaces

3
Can you say Hell?
  • Average surface temperature 4500 C
  • Atmospheric Pressure 90 times Earths
  • No Water
  • Sulfuric Acid Clouds
  • No magnetic field
  • Retrograde rotation
  • Form of tectonism

4
Definition
  • Tectonics is the study of large scale
    processes that collectively deform the planets
    Surface

5
We are in Agreement
  • Venusian surface features are younger than 1 GA
  • Lithosphere relatively thick 200 km
  • No evidence for present day plate tectonics
  • Present day hot spot volcanism

6
Landscape of Venus (Herrick)
  • Venus
  • Tesserae
  • Plains
  • Rift-volcano-coronae zones
  • Earth
  • Continents
  • Oceanic plates
  • Hot spots

7
(No Transcript)
8
Tectonic Models
  • Diapiarism over time (Hansen 2003)
  • Correlation between climate change, surface
    temperature, and Tectonism (Solomon, et al 1999)
  • Subduction to flood basalts to hot spot volcanism
    (Herrick 1992, also Basilevsky and Head 2002)

9
Climate Change Model
  • Large flood basalt volcanic event 700 Ma
  • Greenhouse gases expelled
  • Driving force for surface topography is
    differential between surface temp and mantle temp

10
Diapirism Model
  • Deformation of surface over time by diapirs.
  • Two types
  • Thermal (responsible for larger features crustal
    rises and plateaus)
  • Compositional (responsible for smaller features
    Coronae)
  • Venusian Uniformitarianism

11
Subduction to Hot Spot Model
  • Prior to 800 Ma active subduction and plate
    tectonics
  • Subduction ceased but flood lavas flowed from
    spreading centers (relatively short lived event)
  • Present day hot spot volcanism

12
Conclusions
  • Using earth tectonic and deformation processes
    not a good model
  • Loss of water is key, puts the brakes on
    subduction
  • Low to mid grade metamorphic termperature
    conditions at the surface!
  • No brittle/ductile transition zone, everything
    behaves plastically even at surface
  • The Herrick model is the most likely

13
References
  • Basilevsky, Alexander T., Head, James, W., 2002
  • Hansen, V. L., 2003
  • Herrick, Robert R., 1994
  • Solomon, Sean C., Bullock, Mark A., Grinspoon,
    David H., 1999
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