HR: 0830h
AN: S21F-0401 [PDF]
TI: Crustal Structure of the Tibetan Plateau and Surrounding Area
AU: * Black, J
EM: dragons@orange.net
AF: US Geological Survey, 345 Middlefield Rd., Menlo Park, CA 94025 United States
AU: * Black, J
EM: dragons@orange.net
AF: University of Durham, University Office, Durham, DH1 3HP
United Kingdom
AU: Mooney, W D
EM: mooney@usgs.gov
AF: US Geological Survey, 345 Middlefield Rd., Menlo Park, CA 94025 United States
AB:
In the early Cretaceous (140 Ma), after the break up of Pangea, the Indian and Eurasian plates began moving towards one
another. Initially the movement was accommodated by subduction of oceanic crust and a series of non-terminal collisions with
microplates and arcs. Eventually, at approximately 45 Ma the terminal suture of India and Eurasia began. Since then, the
plates have moved a further 2000 -3000 km together. Scientists are still uncertain as to how and where this crust has been
accommodated. Geological and geophysical data should enable us to answer this and other questions governing the behavior of
the continental crust and deformation processes in operation.
In order to answer these questions and investigate the crustal structure of the area, two datasets have been examined. The
first is a deep seismic profile running northeast across the northeastern flank of the Tibetan Plateau and into the Ordos
Block, part of the Sino-Korean Terrain. The profile is modeled using the reflectivity method. The second dataset compiles
existing data points that comprise velocity-depth information for mid-Asia.
We found that the crust increases in thickness from 40 km in surrounding areas, to 60 km under Tibet. The upper crust is
much thicker than normal (between 40% and 100% thicker). There is no increase in lower crustal thickness, in places there
is no crust with 'normal' lower crustal velocities. The Moho is a complex interface, suggestive of an undulating boundary.
Thickness changes are more sudden along the southern margin of the plateau.
DE: 7205 Continental crust (1242)
DE: 7218 Lithosphere and upper mantle
DE: 8124 Earth's interior--composition and state (old 8105)
DE: 9320 Asia
SC: Seismology [S]
MN: 2003 Fall Meeting