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Rech, J., B. Currie, G. Michalski, and A. Cowan (2006),
Neogene climate change and uplift in the Atacama De-
sert, Chile, Geology, 34(9), 761–764.
Regard, V., M. Saillard, J. Martinod, L. Audin, S. Carre-
tier, K. Pedoja, et al. (2010), Renewed uplift of the Cen-
tral Andes Forearc revealed by coastal evolution during
the Quaternary, Earth and Planetary Science Letters,
2997 (1-2), 199–210.
Rieu, M. (1975), Les formations sédimentaires de la Pampa
del Tamarugal et le Rio Loa. ("Norte Grande" du Chili),
Cah. ORSTOM, sér. Géol., VII (2), 145–164.
Riquelme, R. (2007), Late Cenozoic geomorphologic signal
of Andean forearc deformation and tilting associated
with the uplift and climate changes of the Southern Ata-
cama Desert (26 ◦ S–28 ◦ S), Geomorphology, 86, 283–
306.
Rutland, R. (1971), Andean orogeny and sea floor sprea-
ding, Nature, 233, 252–255.
Sáez, A., A. Cabrera, A. Jensen, and G. Chong (1999),
Late Neogene lacustrine record and palaeogeography in
the Quillagua–Llamara basin, Central Andean fore-arc
(northern Chile), Palaeogeography, Palaeoclimatology,
Palaeoecology, 151, 5–37.
Saillard, M. (2008), Dynamique du soulèvement côtier
Pléistocène des Andes centrales : Etude de l’évolution
géomorphologique et datations (10Be) de séquences de
terrasses marines (Sud Pérou – Nord Chili), Ph.D. the-
sis, Université Paul Sabatier - Toulouse III.
Saillard, M., S. Hall, L. Audin, D. Farber, G. Hérail,
J. Martinod, V. Regard, and R. Finkel (2009), Non-
steady long-term uplift rates and Pleistocene marine
terrace development along the Andean margin of Chile
(31 S) inferred from 10Be dating, Earth and Planetary
Science Letters, 277 (1-2), 1–2.
Salas, R., R. Kast, F. Montecinos, and I. Salas (1966),
Mapa geológico del Departamento de Arica, escala
1 :300.000, Tech. rep., Geología y recursos minerales del
Departamento de Arica, Provincia de Tarapacá.
Bibliographie
Scheuber, E., T. Bogdanic, A. Jensen, and K. Reutter
(1994), Tectonic development of the North Chilean
Andes in relation to plate convergence and magmatism
since the Jurassic, Tectonics of the southern central
Andes, pp. 121–139.
Scheuber, E., K. Hammerschmidt, and H. Friedrichsen
(1995), 40Ar/39Ar and Rb-Sr analyses from ductile
shear zones from the Atacama Fault Zone, northern
Chile : the age of deformation, Tectonophysics, 250, 61–
87.
Schildgen, T., K. Hodges, K. Whipple, P. Reiners, and
M. Pringle (2007), Uplift of the western margin of the
Andean plateau revealed from canyon incision history,
southern Peru, Geology, 35(6), 523–526.
Schildgen, T., K. Hodges, K. Whipple, M. Pringle, M. van
Soest, and K. Cornell (2009), Late Cenozoic structural
and tectonic development of the western margin of the
central Andean Plateau in southwest Peru, Tectonics,
28(4), TC4007.
Schildgen, T., G. Balco, and D. Shuster (2010), Canyon
incision and knickpoint propagation recorded by apa-
tite 4He/3He thermochronometry, Earth and Planetary
Science Letters, 293, 377–387.
Schlunegger, F., G. Zeilinger, A. Kounov, F. Kober, and
B. Husser (2006), Scale of relief growth in the forearc
of the Andes of Northern Chile (Arica latitude, 18 ◦ S),
Terra Nova, 18, 217–223.
Schmitz, M. (1994), A balanced model of the southern Cen-
tral Andes, Tectonics, 13(2), 484–492.
Schmitz, M., W. Heinsohn, and F. Schilling (1997), Seis-
mic, gravity and petrological evidence for partial melt
beneath the thickened Central Andean crust (21-23 ◦ S),
Tectonophysics, 270, 313–326.
Scholl, D., M. Christensen, R. Von Huene, and M. Marlow
(1970), Peru-Chile trench sediments and sea-floor sprea-
ding, Geological Society of America Bulletin, 81(5),
1339–1360.
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