Major tectonic systems Dispersion of the Gondwana continents
- Slides: 35
Major tectonic systems § Dispersion of the Gondwana continents § Closing of Tethys Ocean § Pacific System: rimmed by subduction zones • East Pacific Rise moving towards the Americas • Western Pacific island arcs
Major tectonic systems operating during the past 200 My I. Fragmentation of the Gondwana super-continent § Creation of new Oceans • Atlantic • Indian • circum-Antarctic • formation of passive margins § Closing of Tethys Ocean: • complex Mediterranean – Middle East interactions • major continental collisions in central Asia • Australian-SE Asian collisions
# 18 42. 7 Ma Middle Eocene Drake Passage Indian Pacific connection
#13 35. 5 Ma Early Oligocene Drake Passage Indian Pacific connection
#6, 20. 5 Ma Early Miocene Drake Passage Indian Pacific connection
Drake Passage Indian Pacific connection
Formation of Circum-Antarctic Current >> isolation of Antarctica >> formation of ice sheet circum-Antarctic Current
Formation of North Atlantic Deep water (thermo-haline convection system)
Formation of continental passive margins continental shelf
continental passive margins Sedimentation on subsiding continental shelf thinned continental crust oceanic crust
Major tectonic systems operating during the past 200 My I. Fragmentation of the Gondwana super-continent § Creation of new Oceans • Atlantic • Indian • circum-Antarctic • formation of passive margins § Closing of Tethys Ocean: • complex Mediterranean – Middle East interactions • major continental collisions in central Asia • Australian-SE Asian collisions
Complex intra-continental Mediterranean-central Asian “plate boundary” Earthquake depth 0 -33 km 33 -70 70 -300 300 -700 Indonesian (Sunda. Banda) island arc
Topography for previous slide: note complex topography of Mediterraneancentral Asian “plate boundary”.
India moving northwards
Himalayan evolution
Indention of India into Asia The named dashed and dotted lines represent boundaries between terranes successively accreted to Asia. The accretion increases in age to the north: Indus Tsangbo, 40 Ma Banggong, 160 Ma Jinsha, 200 Ma Kunlun, 255 Ma Tienshan, late Paleozoic The indentation has moved these sutures northwards The dotted areas show the regions of shearing that accomodated the northward indentation of India
Tibetan plateau models
Region of the. Tibetan Plateau Ignore white rectangle. The blue line shows the approximate location of the section shown in the third slide after this one.
A recently published geological cross section See the section line (blue line) on the map shown in the third preceding slide. From Yin, A. and T. M. Harrison, 2000, Geologic Evolution of the Himalayan-Tibetan Orogen, Ann. Rev. Earth Planet. Sci. , v. 28, 211 -280.
Central Asian active tectonics
Major tectonic systems operating during the past 200 My II. Pacific System § East Pacific Rise (EPR) moving towards the Americas and away from Asia § Hot spot tracks §Rimmed by subduction zones • Western Pacific • Subducting old oceanic lithosphere • Formation of back-arc basins and island arcs • Eastern Pacific • Subducting young oceanic lithosphere • Andean type mountain building • Collision and accretion of exotic terranes • Collision of EPR with North America
East c Rise Pacifi
Major tectonic systems operating during the past 200 My II. Pacific System § East Pacific Rise (EPR) moving towards the Americas and away from Asia § Hot spot tracks §Rimmed by subduction zones • Western Pacific • Subducting old oceanic lithosphere • Formation of back-arc basins and island arcs • Eastern Pacific • Subducting young oceanic lithosphere • Andean type mountain building • Collision and accretion of exotic terranes • Collision of EPR with North America
Northwestern Pacific Subduction zones: seismicity Ryukyu island arc Kurile. Kamchatka island arc Aleutian Island arc N. Honshu subduction zone Izu-Bonin. Marianas island arc Earthquake depth 0 -33 km 33 -70 70 -300 300 -700
Northwestern Pacific Subduction zones: bathymetry
New Britain Island arc Southwestern Pacific Subduction zones: seismicity Vanuatu island arc Tonga island arc Kermadec island arc New Zealand Earthquake depth 0 -33 km 33 -70 70 -300 300 -700
Southwestern Pacific Subduction zones: bathymetry
Major tectonic systems operating during the past 200 My II. Pacific System § East Pacific Rise (EPR) moving towards the Americas and away from Asia § Hot spot tracks §Rimmed by subduction zones • Western Pacific • Subducting old oceanic lithosphere • Formation of back-arc basins and island arcs • Eastern Pacific • Subducting young oceanic lithosphere • Andean type mountain building • Collision and accretion of exotic terranes • Collision of EPR with North America
- Gondwana land
- Air gondwana
- Dispersion phase and dispersion medium
- Lyophilic colloids and lyophobic colloids difference
- Intermodal dispersion and intramodal dispersion
- Transform fault
- Population distribution
- Which continent is london
- Rome controlled territory on what three continents?
- The seven continents
- Biggest continet
- How many continents
- Chapter 24 the land where continents collided
- Continents all together
- How many continents are there
- Similar fossils found on different continents
- Evidence for pangea
- Continents change position over time
- Geographical names with and without the
- Outline map of continents and oceans
- Continent vocabulary
- Continents and oceans
- Similar fossils found on different continents
- Label the world's 5 oceans
- Continents facts
- The prime meridian runs through which 3 continents
- Continents and oceans map
- Greek civilization introduction
- Chapter 7 section 2 restless continents answer key
- What continents were involved in the columbian exchange
- Which three continents meet in the middle east
- Continents and oceans song
- Nematath
- Continents and oceans jeopardy
- Continents and oceans jeopardy
- What are the five themes of geography