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GEOG111: LEC 7 - NEW GLOBAL TECTONICS

OCEANIC AND CONTINENTAL CRUST

  • Continental crust (~2.7 g/cm³)

    • largely granite

  • Ocean Crust (~3.0g/cm³)

    • Largely basalt and gabbro

  • Tectonics: the folding and breaking of rocks due to pressure within the earths crust

    • Folding: the bending of crustal rocks, normally due to compression (soft deformation)

    • Faulting: the breaking and resultant displacement of a rock body (brittle deformation)

  • Continental Drift: Wegeners Pangea

    • Modern reconstruction of Pangea

    • Evidence: geologic, climatic, paleontology, shape

    • Critical point missing: doesn’t mention any processes

SEAFLOOR TOPOGRAPHY - MARIE THARP

  • Character of a Divergent margin

    • Plate types: O/O, C/C

    • Applied stress: Extension

    • Resulting strain: Stretching

    • Surface Expression: Low ridge with central trench

    • Seismicity: Low energy, shallow depth

    • Volcanism: Low explosivity, fluid lava

      • Divergent boundary - fast spreading ridge

        • Mid ocean ridge processes:

          • Hot mantle rock risees

          • Melt forms under the lithosphere

          • Magma rises into magma chamber in crust and is injected as dikes forming in new crust

          • law erupts onto ocean floor adding to crust

          • Plates move apart, cool, and thicken

  • Character of a transform margin

    • Plate types: O/O, O/C, C/C

    • Applied stress: shear

    • Resulting strain: shearing/twisting laterally

    • Surface expression: offset surface

    • Seismicity: low to moderate energy, shallow

    • Volcanism: not generally present

How do tectonics play a significant role in recycling rocks

  • Divergent/transform boundaries

    • Driven by convection currents within the earth

  • Different boundaries have different surface expression and geophysical indicators

    • Earthquakes, volcanic activity, trenches, ridges

  • Character of a convergent margin

    • Plates locked = stress and deformation

    • Plates release = earthquake and tsunami

      • Platetypes: O/O, O/C (Subduction)

      • Applied stress: Compression

      • Resulting strain: shortening

      • Resulting expression: trench, uplifted mountains

      • Seismicity: high energy, shallow to very deep

      • Volcanism: high explosivity, thick lava

TERRANE ACCRETION

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GEOG111: LEC 7 - NEW GLOBAL TECTONICS

OCEANIC AND CONTINENTAL CRUST

  • Continental crust (~2.7 g/cm³)

    • largely granite

  • Ocean Crust (~3.0g/cm³)

    • Largely basalt and gabbro

  • Tectonics: the folding and breaking of rocks due to pressure within the earths crust

    • Folding: the bending of crustal rocks, normally due to compression (soft deformation)

    • Faulting: the breaking and resultant displacement of a rock body (brittle deformation)

  • Continental Drift: Wegeners Pangea

    • Modern reconstruction of Pangea

    • Evidence: geologic, climatic, paleontology, shape

    • Critical point missing: doesn’t mention any processes

SEAFLOOR TOPOGRAPHY - MARIE THARP

  • Character of a Divergent margin

    • Plate types: O/O, C/C

    • Applied stress: Extension

    • Resulting strain: Stretching

    • Surface Expression: Low ridge with central trench

    • Seismicity: Low energy, shallow depth

    • Volcanism: Low explosivity, fluid lava

      • Divergent boundary - fast spreading ridge

        • Mid ocean ridge processes:

          • Hot mantle rock risees

          • Melt forms under the lithosphere

          • Magma rises into magma chamber in crust and is injected as dikes forming in new crust

          • law erupts onto ocean floor adding to crust

          • Plates move apart, cool, and thicken

  • Character of a transform margin

    • Plate types: O/O, O/C, C/C

    • Applied stress: shear

    • Resulting strain: shearing/twisting laterally

    • Surface expression: offset surface

    • Seismicity: low to moderate energy, shallow

    • Volcanism: not generally present

How do tectonics play a significant role in recycling rocks

  • Divergent/transform boundaries

    • Driven by convection currents within the earth

  • Different boundaries have different surface expression and geophysical indicators

    • Earthquakes, volcanic activity, trenches, ridges

  • Character of a convergent margin

    • Plates locked = stress and deformation

    • Plates release = earthquake and tsunami

      • Platetypes: O/O, O/C (Subduction)

      • Applied stress: Compression

      • Resulting strain: shortening

      • Resulting expression: trench, uplifted mountains

      • Seismicity: high energy, shallow to very deep

      • Volcanism: high explosivity, thick lava

TERRANE ACCRETION

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