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Geology; September 2003; v. 31; no. 9; p. 797-800; DOI: 10.1130/G19572.1
© 2003 Geological Society of America
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Late Miocene to present exhumation in the Ligurian Alps (southwest Alps) with evidence for accelerated denudation during the Messinian salinity crisis

J.P.T. Foeken1, T.J. Dunai1, G. Bertotti1 and P.A.M. Andriessen1

1 Faculty of Earth and Life Sciences, Vrije Universiteit Amsterdam, 1081HV Amsterdam, The Netherlands

Detrital apatite (U-Th)/He and fission-track thermochronometry are applied to constrain the exhumation history of the Ligurian Alps (southwest Alps). Exhumation of the Ligurian Alps is recorded from ca. 11 Ma and continues until present. More than 4 km of exhumation is recorded at an average rate of 0.4 ± 0.2 mm/yr. Exhumation is accommodated along a north-dipping thrust at the foot of the Ligurian margin. Combined (U-Th)/He and fission-track thermal modeling show a phase of accelerated denudation between 7 and 5 Ma, associated with the base-level drop during the Messinian salinity crisis.

Key Words: (U-Th)/He dating • thermochronology • Messinian salinity crisis • Ligurian Alps




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H. R. Groger, B. Fugenschuh, M. Tischler, S. M. Schmid, and J. P. T. Foeken
Tertiary cooling and exhumation history in the Maramures area (internal eastern Carpathians, northern Romania): thermochronology and structural data
Geological Society, London, Special Publications, January 1, 2008; 298(1): 169 - 195.
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