GEOPH 300: Physics of the Earth Geodynamics (Physics of plate tectonics) – Spherical geometry,...
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Transcript of GEOPH 300: Physics of the Earth Geodynamics (Physics of plate tectonics) – Spherical geometry,...
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GEOPH 300: Physics of the Earth
• Geodynamics (Physics of plate tectonics)– Spherical geometry, reconstruction of plate
motion– Earth’s magnetic field
• Seismology– Earthquake seismology– Active source seismology
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GEOPH 300: Physics of the Earth
• Geochronology– Radioactive decay and useful decay systems
• Heat flow– The earth as a heat engine – total heat generation and
loss from the earth• What geophysics tells about the structure of the
deep interior and the continental and oceanic lithospheres
• Geophysics to study Earth’s climate– Remote sensing, glacier earthquakes
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Geodynamics
• Lithosphere (lithos – rock)– Strong outermost shell including the crust and
uppermost mantle (~100 km)– Thinnest in the oceans, thicker under the
continents• Asthenosphere (asthenia – weak or sick)– High temperature and pressure allow for viscous
flow at geologic timescales
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Geodynamics
• Lithosphere is divide into a small number of rigid plates moving over the asthenosphere– Most deformation takes place along plate edges
• Seismicity outlines the plate boundaries– Seven main plates• Pacific, Antarctic, South American, North American,
African, Eurasian, Indian(see IRIS webpage)
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Geodynamics
• Assumptions of plate tectonics1. Generation of new plate material occurs by sea
floor spreading2. The new oceanic lithosphere becomes part of a
rigid plate that may or may not include continental material
3. The Earth’s surface area remains constant4. Relative motion between plates is
accommodated along plate boundaries
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Geodynamics
• Types of plate boundaries– Divergent (Constructive)• Mid-ocean ridge, material is added to the crust
– Convergent (Destructive)• Subduction zone, material is returned to the mantle
– Conservative• Transform faults – six basic classes
– Most common is ridge-ridge fault
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Source: http://www.mantleplumes.org
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Geodynamics
• We can think of plate motion as relative– Velocity of plate A with respect to plate B is BvA
and B with respect to A is AvB
AvB = - BvA
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Geodynamics
• We use vector addition to determine relative motion between multiple plates– Say we know relative motion between A and B,
and between A and C, we determine motion between B and C by
CvB = CvA + AvB
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Geodynamics
• Plate motion on a sphere– Euler’s fixed point theorem
“The most general displacement of a rigid body with a fixed point is equivalent to a rotation about an axis through that fixed point”
or“Every displacement from one
position to another on the surface of the Earth can be regarded as a rotation about a suitably chosen axis passing through the center of the Earth”
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Geodynamics
• This suitably chosen axis is call the rotation axis and it intersects the surface at two poles of rotation
• Relative velocity between two plates is given by
v=ωRsinθ
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Geodynamics
• Determining rotation poles and rotation vectors– Instantaneous poles of rotation and relative angular velocities
• Snapshot in geologic time
– Strike of active transform faults– Spreading rate along constructive plate boundaries– Focal mechanism analysis– Land displacement surveys– Space based methods
• Satellite laser ranging system• Very-long-baseline interferometry• Geodetic grade GPS
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Source: R. McCaffreyhttp://ees2.geo.rpi.edu/rob/www/gps/g0026.html#fig3
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Payne, S.J., R. McCaffrey, and R.W. King, 2008, Strain rates and contemporary deformation in the Snake River Plain and surrounding Basin and Range from GPS and seismicity: Geology, v. 36, 647-650
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Absolute plate motions – hotspot tracks
http://www.ig.utexas.edu/research/projects/lips/data/hotspots.htm
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The classical model
Geodynamics, Seismology & PlumesGillian R. Foulger
University of Durham, UK
http://www.mantleplumes.org
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The alternative model
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Plume Plate
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Christiansen, R.L., Foulger, G.R., and Evans, J.R., 2002, Upper mantle origin of the Yellowstone hotspot: GSA Bulletin, 114 (10), 1245-1256
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