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How and why does subduction occur?

How and why does subduction occur?. Convergence One plate sinks beneath the other Dense oceanic crust sinks into mantle. What and where is the Wadati-Benioff zone?. Inclined array of earthquakes at subduction zone Correspond to upper edge of plate. How is magma produced at arcs?.

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How and why does subduction occur?

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  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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