Tectonic rotations and transcurrent deformation south
of the Abancay deflection in the Andes of southern Peru
Pierrick Roperch,1
Victor Carlotto,2,3
Gilles Ruffet,4
and Michel Fornari5
Received 14 April 2010; revised 2 January 2011; accepted 11...
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Tectonic rotations and transcurrent deformation south
of the Abancay deflection in the Andes of southern Peru
Pierrick Roperch,1
Victor Carlotto,2,3
Gilles Ruffet,4
and Michel Fornari5
Received 14 April 2010; revised 2 January 2011; accepted 11 January 2011; published 8 April 2011.
[1] We report new paleomagnetic results from 55 out of 76 sites sampled at different
localities along a transect from Nazca to Cuzco where the general structures of the
Peruvian Andes are strongly offset across the Abancay deflection.
Nine new 39
Ar/40
Ar
ages better constrain the timing of volcanism along the western edge of the Western
Cordillera at the latitude of Nazca.
A mean paleomagnetic result from 22 sites in the lower
Miocene volcanics does not show significant rotation (R = −2.
3° ± 7.
7°) of the western
margin of the Central Andean Plateau since the early Miocene.
Within the Western
Cordillera we sampled three structural blocks bounded to the north by the Abancay fault
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