Plate Tectonics: Knowns and Unknowns · • Plate tectonics explains ridges, transforms, subduction...
Transcript of Plate Tectonics: Knowns and Unknowns · • Plate tectonics explains ridges, transforms, subduction...
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Plate Tectonics:Knowns and Unknowns
David Sandwell - SOEST, October 2, 2008
• Knowns: ridges, transforms, subduction zones,propagators, microplates, . . .
• Unknowns: hotspot connection to plumes and origin ofHaxby gravity lineations
How many hotspots are caused by mantle plumes (0 - 49)?
Do Haxby gravity lineations originate in the lithosphere orasthenosphere?
plate tectonics
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What were they smoking in the 60’s?
(Holden, J. C. and P. R. Vogt, Graphic Solutions to Problems of Plumacy, EOS Trans. AGU, 56, 573-560, 1977)
satellite altimetry
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bumps on the surface of the ocean
confirmations and discoveriesfrom satellite altimetry
• confirming/refining plate tectonics
• microplates and propagating ridges
• seafloor roughness versus spreading rate
• global seafloor age
• global bathymetry grids
• seamounts > 2 km tall
• Haxby gravity lineations
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ridges andtransforms
500
km
fracture zones
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subduction zones
triple junction
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back-arc spreading
It is not always this perfect.
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confirmations and discoveriesfrom satellite altimetry
• confirming/refining plate tectonics
• microplates and propagating ridges
• seafloor roughness versus spreading rate
• global seafloor age
• global bathymetry grids
• seamounts > 2 km tall
• Haxby gravity lineations
microplates and overlapping spreading ridges
500 km
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propagating rifts
500 km
confirmations and discoveriesfrom satellite altimetry
• confirming/refining plate tectonics
• microplates and propagating ridges
• seafloor roughness versus spreading rate
• global seafloor age
• global bathymetry grids
• seamounts > 2 km tall
• Haxby gravity lineations
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fast vs. slow spreading
Small and Sandwell, Geology, 1994
fast spreading vs. slow spreading
1000 km
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confirmations and discoveriesfrom satellite altimetry
• confirming/refining plate tectonics
• microplates and propagating ridges
• seafloor roughness versus spreading rate
• global seafloor age
• global bathymetry grids
• seamounts > 2 km tall
• Haxby gravity lineations
fracture zones = spreading direction
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FZ direction + magnetic anomalies = seafloor age[Mueller et al., 1997]
confirmations and discoveriesfrom satellite altimetry
• confirming/refining plate tectonics
• microplates and propagating ridges
• seafloor roughness versus spreading rate
• global seafloor age
• global bathymetry grids
• seamounts > 2 km tall
• Haxby gravity lineations
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seamounts [Wessel, 2001]
USS San Francisco crashed into2-km tall uncharted guyot
• Los Angeles class nuclearsubmarine ran aground inroute from Guam toBrisbane, Australia - 8January, 2005
• One sailor killed, 115injured
• Crash depth ~160 m,speed 33 kn, Sonarmeasured a depth of 2000m 4 minutes before crash
• 30-hour trip back toGuam, crew managed tokeep the sub from sinking
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confirmations and discoveriesfrom satellite altimetry
• confirming/refining plate tectonics
• microplates and propagating ridges
• seafloor roughness versus spreading rate
• global seafloor age
• global bathymetry grids
• seamounts > 2 km tall
• Haxby gravity lineations
gravity lineations and linear volcanic ridges:asthenosphere or lithosphere?
What processes form linear volcanic chains?mantle plumes (upper and lower mantle)cracks in the plate (lithosphere)small scale convection (asthenosphere)
How to crossgrain gravity lineaments form?small scale convection or mantle return flow(asthenosphere)thermal bending or boudinage (lithosphere)
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gravitylineations
Haxby and Weissel,JGR, v. 91, 1986
linear volcanic chains
possible processes:
A) mantle plumes
B) plate boundary forces and thermal stress crack the plate allowingmagma to escape
C) small-scale convection
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Attributes of Mantle Plumes
(Courtillot, Davaille, Besse and Stock, EPSL, v205, 2003.)
1. linear volcanic chain with monotonous age progression
2. flood basalt at origin of track
3. large buoyancy flux
4. consistently high ratios of 3 of 4 isotopes of helium
5. significant low shear wave velocity in underlying mantle.
6. geoid/topography ratio > 2.5 m/km
possibledeep mantle plumes
(Courtillot, Davaille, Besseand Stock, EPSL, v. 205,2003.)
9 hotspots have> 3 attributes
1. Afar2. Caroline3. Easter4. Hawaii5. Iceland6. Louisville7. Reunion8. Samoa9. Tristan
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Haxby and Turcotte, 1978Sandwell and MacKenzie, 1989
low GTR = Airy-compensated plateaus
high GTR = thermally-compensated swells
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separating swells from plateaus (Sandwell and MacKenzie, JGR, v. 94, 1989)
thermalswells
HawaiiIcelandReunion
1. linear volcanic chain with monotonous age progression2. flood basalt at origin of track3. large buoyancy flux4. consistently high ratios of 3 of 4 isotopes of helium5. significant low shear wave velocity in underlying mantle.6. geoid/topography ratio > 2.5 m/km
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Many intraplate features have few plume attributes.
Are these features related to asthenospheric or lithospheric processes?
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What produced these features??
Plate Boundary Forces
Proposed processes:
A) mantle plumes (~3 hotspots have all the attributes)
B) plate boundary forces and thermal stress crack theplate allowing magma to escape
C) small-scale convection
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Plate Driving Forces on Earth
FS - swell pushFD - dragFT - trench pull
Forsyth and Uyeda,GJRAS, 1975
trench pull ≈ 3 x ridge push
(Geology, v.9, 1981)
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Rifting of old oceanic lithosphere is caused by slab pull.
Is the Easter/Salas y Gomez Chain a rift?
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Lithospheric Stresses, Great Fissures, and Volcanism at Seamounts and Plateaus
James H. Natland, and Edward L. Winterer, GSA Penrose Volume, in press, 2005
“We propose that changes in the distribution of large seamounts and oceanislands in the Pacific are closely linked to this history and to the shifting patternsof lithospheric stress imposed on the plate from its boundaries since theMesozoic. The stresses produce great fissures and systems of fissures throughthe plate that root in zones of mantle where partial melting occurs and magmaaccumulates. The fissures thus provide avenues for escape of buoyant magma,thence formation of seamounts, islands, and volcanic ridges. Today, manyfissures propagate, not always at the same rate, in directions immediatelyopposed to the direction of plate motion, and this gives rise to the linearvolcanic chains of the Pacific.”
changes in plate boundary configuration in the past
Haxby gravity lineations
• gravity lineations are common on the Pacific andNazca plates
• they cross the grain of the seafloor spreading fabric
• they are not apparent at the ridge and form in 3-5 Ma
• volcanic ridges are in troughs of gravity lineations
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gravitylineations
Haxby and Weissel,JGR, v. 91, 1986
development of gravity lineations
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volcanic ridges
volcanic ridges
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(Haxby and Weissel, 1986)(Sandwell et al., 1995)
(Gans et al., 2003)
(Weerarante et al., 2003)
(Haxby and Weissel, 1986) (Sandwell et al., 1995)
(Gans et al., 2003)
(Weerarante et al., 2003)
10% extension not observed inFZ spacing(Goodwillie and Parsons, 1992;Gans et al., 2003)
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ridges are in troughs of lineations
(Haxby and Weissel, 1986) (Sandwell et al., 1995)
(Gans et al., 2003)
(Weerarante et al., 2003)
volcanic ridges occur in thetroughs of the gravity lineations
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(Ballmer et al., GRL 2007)
small scale convection
(Ballmer et al., GRL 2007)
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(Haxby and Weissel, 1986) (Sandwell et al., 1995)
(Gans et al., 2003)
(Weerarante et al., 2003)
small scale convection cannot explain formation on lithosphere< 25 Ma.
thermoelastic model can predicts boththe amplitude and wavelength of the gravitylineations
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modeling gravity lineations
• calculate thermoelastic bending moment (Parmentier andHaxby, 1986; Wessel, 1992)
• introduce cracks in the plate and calculate topographyand gravity lineations (Turcotte, 1974; Gans et al, 2003)
• find maximum in thermoelastic energy released versuscrack spacing (Sandwell and Fialko, 2004)
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seagoing proposal – (4th try)
seagoing proposal – (4th try)
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Conclusions
• Plate tectonics explains ridges, transforms, subduction zones,propagators, microplates, . . .
• Plate tectonics makes predictions about the present, past,and future of the Earth.
• How many hotspots were formed by mantle plumes (0 - 49)?
• What causes Haxby gravity lineations and associated linearvolcanic ridges?