How and why does subduction occur? - PowerPoint PPT Presentation

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How and why does subduction occur?

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Dense oceanic crust sinks into mantle. What and where is the Wadati-Benioff zone? ... Deformation intensifies in the core of the orogen (higher T and P) ... – PowerPoint PPT presentation

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Title: How and why does subduction occur?


1
How and why does subduction occur?
  • Convergence
  • One plate sinks beneath the other
  • Dense oceanic crust sinks into mantle

2
What and where is the Wadati-Benioff zone?
  • Inclined array of earthquakes at subduction zone
  • Correspond to upper edge of plate

3
How is magma produced at arcs?
  • Water from subducting slab lowers the melting
    point of overlying mantle
  • Note water also makes for explosive eruptions

4
Where and how do sediments accumulate in arc
environments?
  • Sediments accumulate in accretionary wedges at
    the trench
  • Two sources 1) volcanic arc 2) ocean sediments

5
Describe deformation of the sediment in the trench
  • Bulldozer action scrapes ocean sediments and
    thrusts material into a wedge

6
Briefly explain the orogenic cycle using India as
an example
  • Gondwana rifts into pieces incuding India
  • India diverges from antarctica but converges on
    Asia
  • India sutures to Asia

7
How can continents accumulate additional terrain
via plate convergence?
  • collage tectonics
  • Example The berkshires

8
Have the continents always looked like they do
today?
  • Continents have grown by lateral accretion
  • Average age of continents 2 billion
  • Average age of oceans 100 million
  • Appalachian not at plate boundary

9
Has the mid-continent always been flat?
  • Continental shield have the oldest rocks.
  • Composed of sutured belts of mountains, which
    were eroded to platforms long ago
  • These platforms have harbored shallow seas

10
What happens to the weak upper layers of crust
during collision?
  • Compression results in thrust faulting and
    folding into nappes.
  • Deformation intensifies in the core of the orogen
    (higher T and P)

11
What happens to the weak upper layers of crust
during collision?
  • Compression results in thrust faulting and
    folding into nappes.
  • Deformation intensifies in the core of the orogen
    (higher T and P)
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