evolution/history of the continents chapter 10. spreading center (divergent boundary) subduction...
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EVOLUTION/HISTORY OF THE CONTINENTS
Chapter 10
Spreading center(divergent boundary)
Subduction margin(convergent boundary)
Transformfault
Island arc
Submarine deposits
Ancient ocean floor
Displaced continental fragments
N O R T HA M E R I C A
AleutianTrench
CascadiaTrench
San AndreasFault
Wrangellia
Much of western North America is made up of exotic terranes accreted over the past 200 million years.
Wrangellia was transported from 5000 km away in theSouthern Hemisphere.
ACCRETION OF A BUOYANT FRAGMENT TO A CONTINENT
Continentalcrust
Asthenosphere
Lithosphere
Fragment
Accreted terrane
A buoyant fragment is carried into a plate collision zone.
The fragment is more buoyant than the lithosphere and is not subducted.
The fragment becomes welded to the overriding plate.
ACCRETION OF AN ISLAND ARC TO ACONTINENT
Continentalcrust
Accreted terrane
Island arc
A plate carrying a continent subducts beneath an oceanic island arc.
The continental crust is not subducted.
The island arc crust becomes welded to the continent.
ACCRETION ALONGA TRANSFORM FAULT
Terranefragment
Two plates slide past eachother along a transform fault.
A terrane fragment on plate B is carried along the margin of plate A.
When the fault becomes inactive, the fragment becomes welded far from its original position.
Transformfault
Plate A
Plate B
Terranefragment
Accretedterrane
ACCRETION BYCONTINENTALCOLLISION ANDRIFTING
A plate carrying a continent subducts beneath another continental plate.
The continents are welded together along a set of thrust faults.
Later, rifting and seafloor spreading carry the plates apart, leaving a fragment of one welded to the other.
ContinentalPlate A
ContinentalPlate B
Thrustfaults
Accretedterrane
AtlasMountains Alps Caucasus
ZagrosMountains Tien Shan
TibetanPlateau Himalaya
ASIAEUROPE
AFRICA SaudiArabia India
China
Earthquake depth50 km deep (shallow focus)
50–300 km deep
300 km deep (deep focus)
The African, Arabian, and Indian plates raised chains of mountains as they collided with the Eurasian Plate.
Earthquake activity indicates that this orogeny is still in progress today.
IndianPlate
Paleozoicsediments
Mesozoicsediments
Accretionarywedge
Forearcbasin
EurasianPlate(Tibet)
Continental crust
Oceanic crust Oceanic mantle
lithosphere
60 MaAs the Indian plate subducted under the Eurasian Plate, an accretionary wedge accumulated. Rising magma thickened the Eurasian Plate crust.
Main Central
Thrust
30-50 MaIndia collided with Tibet, breaking along the Main Central Thrust fault.
Main Boundary Fault
20-30 MaAs the collision continued, a slice of India crust was stacked onto the oncoming subcontinent.
Main Central Thrust
Eroded uplifted material
Main BoundaryFault
10-20 MaA second thrust fault developed, stacking a second slice of crust onto India and lifting the first slice. These overthrust slices make up the bulk of the Himalaya.
Main Central Thrust
Himalaya Tibetan PlateauGanges Plain
Equator
IAPETUSOCEAN
LAURENTIA
BALTICA
Middle Cambrian (510 Ma)After the breakup of Rodinia, the continent ofLaurentia straddled the equator.
Equator
IAPETUSOCEAN
LAURENTIA BALTICA
Late Ordovician (450 Ma)An island arc collided with Laurentia, causing the Taconic orogeny.
Taco
nic
orogeny
LAURUSSIA
GONDWANA
Early Devonian (400 Ma)The collision of Laurentia with the continent ofBaltica formed Laurussia.
Caledonianorogeny
Acadianorogeny
LAURUSSIA
GONDWANA
Late Mississippian (340 Ma)The collision of Gondwana with Laurussia beganwith the Variscan orogeny…
Variscanorogeny
Shelf andsubmergedcontinent
Equator
GONDWANA
Upper Pennsylvanian (300 Ma)… and continued with the Appalachian orogeny.Siberia converged with Laurussia to form Laurasia.
Variscanorogeny
Equator
LAURUSSIA
Hercynian
orogeny
Appalachianorogeny
Uralorogeny
GONDWANA
Early Permian (270 Ma)The end product was the supercontinentof Pangaea.
Equator LAURASIA
Uralorogeny
Rifting splits the continent...
Supercontinent Cycle
…leading to the creation of new oceanic crust.
Passive margin cooling occurs and sedimentaccumulates.
Convergence begins: an oceanic plate subductsbeneath a continental plate, creating avolcanic chain.
Terrane accretion welds material to the continent.
Orogeny thickens the crust and buildsmountains, forming a new supercontinent.
The continent erodes, thinning the crust. Riftingmay begin the process again.