Articles | Volume 3, issue 1
Special issue:
Research article
22 Feb 2012
Research article |  | 22 Feb 2012

Effect of glacial-interglacial sea-level changes on the displacement and stress field in the forearc and along the plate interface of subduction zones

T. Li and A. Hampel

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Cited articles

Adam, J., Kläschen, D., Kukowski, N., and Flüh, E.: Upward delamination of Cascadia Basin sediment infill with landward frontal accretion thrusting caused by rapid glacial age material flux, Tectonics, 23, TC3009,, 2004.
Bard, E., Hamelin, B., Fairbanks, R. G., and Zindler, A.: U-Th ages from mass spectrometry in corals from Barbados: sea level during the past 130 000 years, Nature, 346, 456–458, 1990.
Blumberg, S., Lamy, F., Arz, H. W., Echtler, H. P., Wiedicke, M., Haug, G. H., and Oncken, O.: Turbiditic trench deposits at the South-Chilean active margin: A Pleistocene–Holocene record of climate and tectonics, Earth Planet. Sci. Lett., 268, 526–539,, 2008.
Bourgois, J., Guivel, C., Lagabrielle, Y., Calmus, T., Boulegue, J., and Daux, V.: Glacial-interglacial trench supply variation, spreading-ridge subduction, and feedback controls on the Andean margin development at the Chile triple junction area (45–48° S), J. Geophys. Res., 105, 8355–8386, 2000.
Buiter, S. J. H., Govers, R., and Wortel, M. J. R.: A modelling study of vertical surface displacements at convergent plate margins, Geophys. J. Int. 147, 415–427, 2001.
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