TY  - JOUR
A1  - Hain, Mathis P.
A1  - Strecker, Manfred
A1  - Bookhagen, Bodo
A1  - Alonso, Ricardo N.
A1  - Pingel, H.
A1  - Schmitt, Axel K.
T1  - Neogene to quaternary broken foreland formation and sedimentation dynamics in the Andes of NW Argentina (25 degrees S)
JF  - Tectonics
N2  - The northwest Argentine Andes constitute a premier natural laboratory to assess the complex interactions between isolated uplifts, orographic precipitation gradients, and related erosion and sedimentation patterns. Here we present new stratigraphic observations and age information from intermontane basin sediments to elucidate the Neogene to Quaternary shortening history and associated sediment dynamics of the broken Salta foreland. This part of the Andean orogen, which comprises an array of basement-cored range uplifts, is located at similar to 25 degrees S and lies to the east of the arid intraorogenic Altiplano/Puna plateau. In the Salta foreland, spatially and temporally disparate range uplift along steeply dipping inherited faults has resulted in foreland compartmentalization with steep basin-tobasin precipitation gradients. Sediment architecture and facies associations record a three-phase (similar to 10, similar to 5, and <2 Ma), east directed, yet unsystematic evolution of shortening, foreland fragmentation, and ensuing changes in precipitation and sediment transport. The provenance signatures of these deposits reflect the trapping of sediments in the intermontane basins of the Andean hinterland, as well as the evolution of a severed fluvial network. Present-day moisture supply to the hinterland is determined by range relief and basin elevation. The conspiring effects of range uplift and low rainfall help the entrapment and long-term storage of sediments, ultimately raising basin elevation in the hinterland, which may amplify aridification in the orogen interior.
Y1  - 2011
U6  - https://doi.org/10.1029/2010TC002703
SN  - 0278-7407
VL  - 30
IS  - 11
PB  - American Geophysical Union
CY  - Washington
ER  - 
TY  - JOUR
A1  - Garcia, Victor H.
A1  - Hongn, Fernando D.
A1  - Yagupsky, Daniel
A1  - Pingel, Heiko
A1  - Kinnaird, Timothy
A1  - Winocur, Diego
A1  - Cristallini, Ernesto
A1  - Robinson, Ruth Aj
A1  - Strecker, Manfred
T1  - Late Quaternary tectonics controlled by fault reactivation. Insights from a local transpressional system in the intermontane Lerma valley, Cordillera Oriental, NW Argentina
JF  - Journal of structural geology
N2  - We analyzed the Lomas de Carabajal area in the intermontane Lerma valley of the Cordillera Oriental to assess the level of neotectonic activity in a densely populated region of northwestern Argentina. In this region, Plio-Pleistocene synorogenic conglomerates are deformed, locally associated with high-angle faults, and NNW-SSE oriented en-echelon folds characterized by wavelengths of < 1 km. The deformed Quaternary units follow the same pattern of deformation as observed in the underlying Neogene deposits; growth-strata geometries are observed near faults. This configuration is compatible with local left-lateral transpressional tectonism driven by ENE-WSW buttressing against the NW-oriented border of a Cretaceous extensional basin (Alemania sub-basin). Optically Stimulated Luminescence analysis of sandy-silty layers interbedded within the folded late Pleistocene conglomeratic sequence helps to determine uplift rates of 0.83-0.87 mm/a during the last 30-40 ka. Nearby the Lomas de Carabajal, a WNW-striking, 3-m-high fault scarp disrupts radiocarbon dated, 10-ka-old loessic deposits providing a Holocene mean uplift rate of 0.30 mm/a. Our data unambiguously show that shallow crustal deformation in the intermontane Lerma valley is ongoing; some of this deformation may be associated with seismicity. Our findings support the notion of temporally and spatially disparate deformation processes in the broken foreland of the northwestern Argentinean Andes.
KW  - Structural geology
KW  - Neotectonics
KW  - OSL and C-14 geochronology
KW  - Syntectonic sedimentation
KW  - Seismogenic sources
Y1  - 2019
U6  - https://doi.org/10.1016/j.jsg.2019.103875
SN  - 0191-8141
VL  - 128
PB  - Elsevier
CY  - Oxford
ER  -