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  • 551.8  (2)
  • Age, 14C calibrated, IntCal13 with Bacon 2.2 (Blaauw and Christen, 2011); Age, maximum/old; Age, minimum/young; Age model; Center for Marine Environmental Sciences; CONDOR-Ia; Depth, corrected; DEPTH, sediment/rock; GeoB3304-5; Gravity corer (Kiel type); MARUM; Number of turbidites; SL; SO101; Sonne; South-East Pacific; Turbidite thickness  (1)
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  • 1
    Publication Date: 2023-06-27
    Keywords: Age, 14C calibrated, IntCal13 with Bacon 2.2 (Blaauw and Christen, 2011); Age, maximum/old; Age, minimum/young; Age model; Center for Marine Environmental Sciences; CONDOR-Ia; Depth, corrected; DEPTH, sediment/rock; GeoB3304-5; Gravity corer (Kiel type); MARUM; Number of turbidites; SL; SO101; Sonne; South-East Pacific; Turbidite thickness
    Type: Dataset
    Format: text/tab-separated-values, 595 data points
    Location Call Number Limitation Availability
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  • 2
    Publication Date: 2021-07-04
    Description: The thick‐skinned fold‐and‐thrust belt on the eastern flank of the Andean Plateau in northwestern Argentina (NWA) is a zone of active contractional deformation characterized by fault‐bounded mountain ranges with no systematic spatiotemporal pattern of tectonic activity. In contrast, the thin‐skinned Subandean fold‐and‐thrust belt of northern Argentina and southern Bolivia is characterized primarily by in‐sequence (i.e., west to east) fault progression, with a narrow zone of Quaternary deformation focused at the front of the orogenic wedge. To better understand how recent deformation is accommodated across these mountain ranges and the Argentinian portion of the orogen in particular, estimating and comparing deformation rates and patterns across different timescales is essential. We present Late Pleistocene shortening rates for the central Calchaquí intermontane valley in NWA associated with at least three episodes of deformation. Global Positioning System data for the same region reveal a gradual decrease in horizontal surface velocities from the Eastern Cordillera toward the foreland, which contrasts with the rapid velocity gradient associated with a locked décollement in the Subandean Ranges of southern Bolivia. Our new results represent a small view of regional deformation that, when considered in combination with the shallow crustal seismicity and decadal‐scale surface velocities, support the notion that strain release in NWA is associated with numerous slowly deforming structures that are distributed throughout the orogen.
    Description: Key Points: Analysis of deformation in northwestern Argentina reveals that numerous, widely distributed, localized structures accommodate shortening. No well‐defined deformation front or clear indication of a locked décollement underlying the region exists. This behavior is fundamentally different from the thin‐skinned fold‐and‐thrust belt of southern Bolivia and northernmost Argentina.
    Description: German Research Foundation (DFG)
    Description: CONICET (Consejo Nacional de Investigaciones Científicas y Técnicas) http://dx.doi.org/10.13039/501100002923
    Keywords: 551.8 ; Subandean fold‐and‐thrust belt ; deformation anlysis
    Type: article
    Location Call Number Limitation Availability
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  • 3
    Publication Date: 2021-09-29
    Description: Complex, time‐dependent, and asymmetric rift geometries are observed throughout the East African Rift System (EARS) and are well documented, for instance, in the Kenya Rift. To unravel asymmetric rifting processes in this region, we conduct 2D geodynamic models. We use the finite element software ASPECT employing visco‐plastic rheologies, mesh‐refinement, distributed random noise seeding, and a free surface. In contrast to many previous numerical modeling studies that aimed at understanding final rifted margin symmetry, we explicitly focus on initial rifting stages to assess geodynamic controls on strain localization and fault evolution. We thereby link to geological and geophysical observations from the Southern and Central Kenya Rift. Our models suggest a three‐stage early rift evolution that dynamically bridges previously inferred fault‐configuration phases of the eastern EARS branch: (1) accommodation of initial strain localization by a single border fault and flexure of the hanging‐wall crust, (2) faulting in the hanging‐wall and increasing upper‐crustal faulting in the rift‐basin center, and (3) loss of pronounced early stage asymmetry prior to basinward localization of deformation. This evolution may provide a template for understanding early extensional faulting in other branches of the East African Rift and in asymmetric rifts worldwide. By modifying the initial random noise distribution that approximates small‐scale tectonic inheritance, we show that a spectrum of first‐order fault configurations with variable symmetry can be produced in models with an otherwise identical setup. This approach sheds new light on along‐strike rift variability controls in active asymmetric rifts and proximal rifted margins.
    Description: Key Points: 2D numerical models elucidate evolution of asymmetric Kenya Rift segments. Intrabasinal faulting is caused by bending of the central block and does not reach the brittle‐ductile transition. Small‐scale crustal inheritance can exert decisive control on first‐order rift architecture.
    Description: Helmholtz Young Ivestigators Group
    Description: National Science Foundation
    Keywords: 551.8 ; 556 ; asymmetric rifting ; rift variability ; numerical model ; structural inheritance ; Kenya Rift
    Type: map
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