Uplift of the Transantarctic Mountains
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The 3,000-km long and 4.5 km high
Transantarctic Mountains represent
the uplifted flank of the
West Antarctic Rift system and mark the
morphological and geological
boundary between East and West
Antarctica. However, the mechanism of
their uplift is not well
understood. The project will use magnetic,
gravity and seismic survey
data to determine the geometry of strata
in the sedimentary basins
beneath southern McMurdo Sound, Antarctica
(the hanging wall) and use
this data to test between various proposed
uplift mechanisms. Some of
the data has already been collected and is
available. Additional data
will be collected in November-December,
2001. The project will
involve data processing and computer modelling
of magnetic and
gravity data and combining this with existing
seismic data. Project
could involve fieldwork during November-December
2001 (to be
negotiated).
Selected References
Behrendt, L.R., S.A. Henrys, J.B. Anderson, and P.J. Barrett, Patterns
of late Cenozoic volcanic and tectonic activity in the West
Antarctic rift system revealed by aeromagnetic surveys, Tectonics,
15, 660-676, 1996.
Fitzgerald, P.F., The Transantarctic Mountains of southern Victoria
land: the application of apatite fission track analysis to a rift
shoulder uplift, Tectonics, 11, 634-662, 1992.
Stern, T.A., and U.S. ten_brink, Flexural uplift of the
Transantarctic Mountains, J. Geophys. Res., 94, 10,315-10,330,
1989.
Stern, T.A., F.J. Davey, and G. Delisle, Lithospheric flexure
induced by the load of the Ross Archipelago, southern Victoria
land, Antarctica, in Geological evolution of Antarctica, edited
by M.R.A. Thomson, A. Crame, and J.W. Thomson, pp. 323-328,
Cambridge University Press, 1991.
Sugden, D.E., G.H. Denton, and D.R. Marchant, Landscape evolution
of the Dry Valleys, Transantarctic Mountains: tectonic implications,
J. Geophys. Res., 100, 9949-9967, 1993.
ten Brink, U., and T. Stern, Rift Flank Uplifts and Hinterland
basins: Comparison of the Transantarctic Mountains with the Great
Escarpment of Southern Africa, J. Geophys. Res., 97, 569-585,
1992.