Relevant bibliographies by topics / Andean fold-thrust

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  1. Journal articles
  2. Dissertations / Theses
  3. Book chapters
  4. Conference papers

Academic literature on the topic 'Andean fold-thrust'

Author: Grafiati
Published: 4 June 2021
Last updated: 1 February 2022

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Journal articles on the topic "Andean fold-thrust"

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McQuarrie, Nadine, Brian K. Horton, George Zandt, Susan Beck, and Peter G. DeCelles. "Lithospheric evolution of the Andean fold–thrust belt, Bolivia, and the origin of the central Andean plateau." Tectonophysics 399, no. 1-4 (2005): 15–37. http://dx.doi.org/10.1016/j.tecto.2004.12.013.

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PEREZ, NICHOLAS D., BRIAN K. HORTON, NADINE McQUARRIE, KONSTANZE STÜBNER, and TODD A. EHLERS. "Andean shortening, inversion and exhumation associated with thin- and thick-skinned deformation in southern Peru." Geological Magazine 153, no. 5-6 (2016): 1013–41. http://dx.doi.org/10.1017/s0016756816000121.

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AbstractA balanced cross-section spanning the Eastern Cordillera and Subandean Zone of southern Peru (13–15°S) constrains ~130 km (38%) of Cenozoic orogen-normal SW–NE Andean deformation accommodated by thick- and thin-skinned retro–arc fold–thrust belt shortening that overprinted pre-Andean Triassic normal faults. Zircon and apatite (U–Th)/He ages demonstrate continuous Oligocene to Miocene cooling of the Permo-Triassic Coasa pluton in the Eastern Cordillera. Zircon (U–Th)/He ages (~34–18 Ma) are reset and define a steep age versus elevation relationship. Apatite (U–Th)/He results reveal reset ages that define two spatially separated groups with ages of ~30–26 Ma and ~17–11 Ma. Detrital zircon U–Pb geochronologic results from Cretaceous–Cenozoic siliciclastic rocks from the Altiplano/Eastern Cordillera record Andean fold–thrust belt and magmatic-arc sediment sources. Correlative Subandean Zone rocks preserve a cratonic sediment contribution, with minor Andean sediment appearing in some Cenozoic rocks. We propose that earliest Andean deformation and structural compartmentalization of the Eastern Cordillera was linked to selective inversion of inherited Permo-Triassic basement-involved normal faults that guided subsequent thick- and thin-skinned deformation. Provenance variations between the hinterland and foreland depocentres reveal competing eastern and western sediment sources, reflecting an axial zone in the Eastern Cordillera that coincided with the inherited Triassic graben and impeded sediment source mixing. Our zircon and apatite (U–Th)/He ages are consistent with published constraints along strike and support pulses of Eocene to late Miocene exhumation that were likely driven by normal fault reactivation and protracted Eastern Cordillera deformation.
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Jackson, Lily J., Brian K. Horton, and Cristian Vallejo. "Detrital zircon U-Pb geochronology of modern Andean rivers in Ecuador: Fingerprinting tectonic provinces and assessing downstream propagation of provenance signals." Geosphere 15, no. 6 (2019): 1943–57. http://dx.doi.org/10.1130/ges02126.1.

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Abstract Recognizing detrital contributions from sediment source regions is fundamental to provenance studies of active and ancient orogenic settings. Detrital zircon U-Pb geochronology of unconsolidated sands from modern rivers that have source catchments with contrasting bedrock signatures provides insight into the fidelity of U-Pb age signatures in discriminating tectonic provenance and downstream propagation of environmental signals. We present 1705 new detrital zircon U-Pb ages for 15 samples of unconsolidated river sands from 12 modern rivers over a large spatial extent of Ecuador (∼1°N–5°S and ∼79°–77°W). Results show distinctive U-Pb age distributions with characteristic zircon age populations for various tectonic provinces along the Andean convergent margin, including the forearc, magmatic arc, and internal (hinterland) and external (foreland) segments of the fold-thrust belt. (1) Forearc and magmatic arc (Western Cordillera) river sands are characterized by Neogene–Quaternary age populations from magmatic sources. (2) Rivers in the hinterland (Eastern Cordillera) segment of the Andean fold-thrust belt have substantial populations of Proterozoic and Paleozoic ages, representing upper Paleozoic–Mesozoic sedimentary and metasedimentary rocks of ultimate cratonic origin. (3) River sands in the frontal fold-thrust belt (Subandean Zone to Oriente Basin) show distinctive bimodal Jurassic age populations, a secondary Triassic population, and subordinate Early Cretaceous ages representative of Mesozoic plutonic and metamorphic bedrock. Detrital zircon U-Pb results from a single regional watershed (Rio Pastaza) spanning the magmatic arc to foreland basin show drastic downstream variations, including the downstream loss of magmatic arc and hinterland signatures and abrupt introduction and dominance of selected sources within the fold-thrust belt. Disproportionate contributions from Mesozoic crystalline metamorphic rocks, which form high-elevation, high-relief areas subject to focused precipitation and active tectonic deformation, are likely the product of focused erosion and high volumes of local sediment input from the frontal fold-thrust belt, leading to dilution of upstream signatures from the hinterland and magmatic arc.
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SUÁREZ, M., R. DE LA CRUZ, and C. M. BELL. "Timing and origin of deformation along the Patagonian fold and thrust belt." Geological Magazine 137, no. 4 (2000): 345–53. http://dx.doi.org/10.1017/s0016756800004192.

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The Andean orogeny in the Patagonian Cordillera of southern South America reflects the consequences of the Mesozoic and Cenozoic subduction of an oceanic plate beneath the South American continental margin. The geological evolution of the region has been influenced by the Eocene collision and subduction of the Farallon–Aluk Ridge and the Miocene–Recent subduction of the Chile Ridge. Another aspect of plate interaction during this period was two intervals of rapid plate convergence, one at 50–42 Ma, and the other at 25–10 Ma, between the South American and the oceanic plates. It has been proposed that the collision of the Chile Ridge with the trench was responsible for the development, at least in part, of the Patagonian fold and thrust belt. This belt extends for more than 1000 km along the eastern foothills of the southern Andes between 46° and 54° S along the southwestern rim of the Austral Basin. The interpretation of a link between subduction of the ridge and formation of the fold and thrust belt is based on assumed time coincidences between contractional tectonism and the collision of ridge segments during Middle and Late Miocene times. The main Tertiary contractional events in the Patagonian fold and thrust belt took place during latest Cretaceous–Palaeocene–Eocene and during Miocene times. Although the timing of deformation is still poorly constrained, the evidence currently available suggests that there is little or no relationship between the timing of the fold and thrust belt and the collision of ridge segments. Most if not all of the contractional tectonism pre-dated the latest episodes of ridge collision. Collision of a ridge crest with the continental margin has been active for the past 14 to 15 million years. Contrary to the suggestion of a relationship between ridge subduction and compression, the main result of this collision has been fast uplift and extensional tectonism. The initiation of the Patagonian fold and thrust belt in latest Cretaceous or early Tertiary times coincided with a fundamental change in the tectonic evolution of the Austral Basin. Throughout the Cretaceous most of this basin subsided as a broad backarc continental shelf. Only in latest Cretaceous times, and coinciding with the initiation of the fold and thrust belt, the basin underwent a transition to a retro-arc foreland basin. This change to an asymmetrically subsiding foreland basin, with an associated foreland fold and thrust belt, was related to uplift of the Andean orogenic belt in the west.
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Husson, Laurent, and Isabelle Moretti. "Thermal regime of fold and thrust belts—an application to the Bolivian sub Andean zone." Tectonophysics 345, no. 1-4 (2002): 253–80. http://dx.doi.org/10.1016/s0040-1951(01)00216-5.

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Echavarria, L., R. Hernández, R. Allmendinger, and J. Reynolds. "Subandean thrust and fold belt of northwestern Argentina: Geometry and timing of the Andean evolution." AAPG Bulletin 87, no. 6 (2003): 965–85. http://dx.doi.org/10.1306/01200300196.

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Zapata, T., and A. Folguera. "Tectonic evolution of the Andean Fold and Thrust Belt of the southern Neuquén Basin, Argentina." Geological Society, London, Special Publications 252, no. 1 (2005): 37–56. http://dx.doi.org/10.1144/gsl.sp.2005.252.01.03.

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BRANELLEC, M., B. NIVIÈRE, J. P. CALLOT, and J. C. RINGENBACH. "Mechanisms of basin contraction and reactivation in the basement-involved Malargüe fold-and-thrust belt, Central Andes (34–36°S)." Geological Magazine 153, no. 5-6 (2016): 926–44. http://dx.doi.org/10.1017/s0016756816000315.

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AbstractWe have conducted a structural study of both the basement-involved Malargüe fold-and-thrust belt (MFTB) and the active San Rafael Block (SRB), which are located in the Central Andes at latitude 34–36°S. Based on several field examples located both in the inner and frontal part of belt and from the distal foreland zone, we focus on the relationships between basement and cover deformation with respect to the known palaeogeography and structural inheritance. In several zones, we point out similarities in the structural and sedimentary responses to Andean shortening. The recent morphologic response has also been investigated through the analysis of active deformation along the eastern border of the SRB. We show that these structural and sedimentary processes are continuous in time and space since they can be applied in the various parts of the fold belt and also at different stages of fold-and-thrust-belt building as well. Finally, we propose the illustration of those mechanisms by complete cross-section along the Rio Grande valley and a possible kinematic scenario of deformation propagation.
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FUENTES, FACUNDO, BRIAN K. HORTON, DANIEL STARCK, and ANDRÉS BOLL. "Structure and tectonic evolution of hybrid thick- and thin-skinned systems in the Malargüe fold–thrust belt, Neuquén basin, Argentina." Geological Magazine 153, no. 5-6 (2016): 1066–84. http://dx.doi.org/10.1017/s0016756816000583.

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AbstractAndean Cenozoic shortening within the Malargüe fold–thrust belt of west-central Argentina has been dominated by basement faults largely influenced by pre-existing Mesozoic rift structures of the Neuquén basin system. The basement contractional structures, however, diverge from many classic inversion geometries in that they formed large hanging-wall anticlines with steeply dipping frontal forelimbs and structural relief in the order of several kilometres. During Cenozoic E–W shortening, the reactivated basement faults propagated into cover strata, feeding slip to shallow thrust systems that were later carried in piggyback fashion above newly formed basement structures, yielding complex thick- and thin-skinned structural relationships. In the adjacent foreland, Cenozoic clastic strata recorded the broad kinematic evolution of the fold–thrust belt. We present a set of structural cross-sections supported by regional surface maps and industry seismic and well data, along with new stratigraphic information for associated Neogene synorogenic foreland basin fill. Collectively, these results provide important constraints on the temporal and geometric linkages between the deeper basement faults (including both reactivated and newly formed structures) and shallow thin-skinned thrust systems, which, in turn, offer insights for the understanding of hydrocarbon systems in the actively explored Neuquén region of the Andean orogenic belt.
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Folguera, Andrés, Víctor A. Ramos, Tomás Zapata, and Mauro G. Spagnuolo. "Andean evolution at the Guañacos and Chos Malal fold and thrust belts (36°30′–37°s)." Journal of Geodynamics 44, no. 3-5 (2007): 129–48. http://dx.doi.org/10.1016/j.jog.2007.02.003.

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Dissertations / Theses on the topic "Andean fold-thrust"

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Podmore, Kevin. "Fluid flow in the Sub Andean fold and thrust belt, Bolivia." Thesis, Keele University, 2013. http://eprints.keele.ac.uk/3867/.

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Understanding fluid flow in fold and thrust belts has the potential to offer enormous insight into hydrocarbon accumulations in regions dominated by such structurally complex settings. Thrusting episodes can be key in creating a complete petroleum system, aiding maturation through burial, developing trapping scenarios, creating pathways for flow though juxtaposition and acting as conduits for flow connecting source to reservoir. The ability to model thrust and fold belts is limited due to the complex nature of threedimensional modelling of thrusts. However recent advancements is structural modelling software have allowed the representation of a stratigraphical surface in two depth locations at a single surface location enabling better realisations of overlain strata in thrust zones. This work simulates the migration of hydrocarbons through fold and thrust zones using new Earth Models of the southern Sub Andean in Bolivia, created from seismic interpretation and well data analysis, and develops a new modelling workflow using multiple geological modelling applications. The migration pathways have been simulated in three dimensions using invasion percolation hydrocarbon migration modelling techniques developed by the Basin Dynamics Research Group at Keele University. These techniques allow the investigation of the relationship of stratal flow properties across thrust blocks. The methodology employed allowed the geological uncertainty of the prospect to be evaluated for hydrocarbon trapping potential, through repeatable simulations where the location point of hydrocarbon source could be controlled. The results of the modelling work provides an insight into the evolution, maturation and potential accumulation of fluids in the Bolivian case study, and has produced a predictive approach to analysing fluid flow and accumulation applicable to other hydrocarbon systems as well as application in other fields considering fluid migration pathways and accumulation.
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Siks, Benjamin Charles. "Sedimentary, structural, and provenance record of the Cianzo basin, Puna plateau-Eastern Cordillera boundary, NW Argentina." Thesis, 2011. http://hdl.handle.net/2152/ETD-UT-2011-05-3449.

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The fault-bounded Cianzo basin represents a Cenozoic intermontane depocenter between the Puna plateau and Eastern Cordillera of the central Andean fold-thrust belt in northern Argentina. New characterizations of fold-thrust structure, nonmarine sedimentation, and sediment provenance for the shortening-induced Cianzo basin at 23°S help constrain the origin, interconnectedness, and subsequent uplift and exhumation of the basin, which may serve as an analogue for other intermontane hinterland basins in the Andes. Structural mapping of the Cianzo basin reveals SW and NE-plunging synclines within the >6000 m-thick, upsection coarsening Cenozoic clastic succession in the shared footwall of the N-striking, E-directed Cianzo thrust fault and transverse, NE-striking Hornocal fault. Growth stratal relationships within upper Miocene levels of the succession indicate syncontractional sedimentation directly adjacent to the Hornocal fault. Measured stratigraphic sections and clastic sedimentary lithofacies of Cenozoic basin-fill deposits show upsection changes from (1) a distal fluvial system recorded by vi fine-grained, paleosol-rich, heavily bioturbated sandstones and mudstones (Paleocene‒Eocene Santa Bárbara Subgroup, ~400 m), to (2) a braided fluvial system represented by cross-stratified sandstones and interbedded mudstones with 0.3 to 8 m upsection-fining sequences (Upper Eocene–Oligocene Casa Grande Formation, ~1400 m), to (3) a distributary fluvial system in the distal sectors of a distributary fluvial megafan represented by structureless sheetflood sandstones, stratified pebble conglomerates and sandstones, and interbedded overbank mudstones (Miocene Río Grande Formation, ~3300 m), to (4) a proximal alluvial fan system with thick conglomerates interbedded with thin discontinuous sandstone lenses (upper Miocene Pisungo Formation, ~1600 m). New 40Ar/39Ar geochronological results for five interbedded volcanic tuffs indicate distributary fluvial deposition of the uppermost Río Grande Formation from 16.31 ± 0.6 Ma to 9.69 ± 0.05 Ma. Sandstone petrographic results show distinct upsection trends in lithic and feldspar content in the Casa Grande, Río Grande, and Pisungo formations, potentially distinguishing western magmatic arc (Western Cordillera) sediment sources from evolving eastern thrust-belt sources (Puna‒Eastern Cordillera). In addition to growth stratal relationships and 40Ar/39Ar constraints, conglomerate clast compositions reflect distinct lithologic differences, constraining the activation of the Cianzo thrust and coeval movement on the reactivated Hornocal fault. Finally, U-Pb geochronological analyses of sandstone detrital zircon populations in conjunction with paleocurrent data and depositional facies patterns help distinguish localized sources from more distal sources west of the basin, revealing a systematic eastward advance of Eocene to Miocene fold-thrust deformation in the central Andes of northern Argentina.<br>text
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Betka, Paul Michael. "Structure of the Patagonian fold-thrust belt in the Magallanes region of Chile, 53° - 55° S Lat." 2013. http://hdl.handle.net/2152/23239.

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The southern Patagonian Andes record the Late Cretaceous closure and inversion of the Late Jurassic – Early Cretaceous Rocas Verdes marginal basin, subsequent development of the Patagonian retroarc fold-thrust belt and the Neogene to present tectonic superposition of a left-lateral strike-slip plate margin defined by the Magallanes- Fagnano fault zone. In this dissertation, I present new geologic maps, cross sections and detailed macro- and microscopic structural analyses that describe the geometry and kinematic evolution of the fold-thrust belt and superposed strike-slip deformation over ~200 km along-strike between 53° and 55° S latitude. Results are discussed in the context of the regional tectonic development of the southernmost Andes and are relevant to the understanding of important tectonic processes including the development of a retroarc fold-thrust belt, the formation of a basal décollement below and toward the hinterland of a fold-thrust belt and the spatial distribution of deformation along a strike-slip plate margin. New maps and balanced cross-sections of the Patagonian fold-thrust belt show that it developed during two main phases of Late Cretaceous to Paleogene shortening that were partly controlled by the antecedent geology and mechanical stratigraphy of the Rocas Verdes basin. During the Late Cretaceous, a thin-skinned thrust belt developed above a décollement that formed first in relatively weak shale deposits of the Rocas Verdes basin and later deepened to <1 km below the basement-cover contact. Ramps that cut mechanically rigid volcanic rocks of the marginal basin link the two décollements. Basement-involved reverse faults that cut the early décollements and probably reactivate Jurassic normal faults reflect Paleogene shortening. Shortening estimates increase northwest to southeast from 26 to 37% over 100 km along-strike and are consistent with regional models of the fold-thrust belt. Structural data, kinematic analyses, and microstructural observations from the lower décollement show that it is defined by transposition of several generations of northeast-vergent noncylindrical folds, shear bands, and a quartz stretching lineation that are kinematically compatible with first-generation structures of the fold-thrust belt. Quartz microstructural data from the décollement are consistent with deformation temperatures that decrease from ~500-650° C to ~400-550° C over ~75 km in the transport direction, indicating that the décollement dipped shallowly (~6°) toward the hinterland. The décollement decoupled the underthrust continental margin from the fold- thrust belt and exemplifies the kinematic relationship between shortening that occurs coevally in a retroarc fold thrust-belt and its polydeformed metamorphic ‘basement’. Fault kinematic data and crosscutting relationships show kinematic and temporal relationships between populations of thrust, strike-slip and normal faults that occur in the study area. Thrust faults form an internally compatible population that shows subhorizontal northeast-trending shortening of the fold-thrust belt and is kinematically distinct from populations of normal and strike-slip faults. Both strike-slip and normal faults crosscut the fold-thrust belt, are localized near segments of the Magallanes- Fagnano fault zone, have mutually compatible kinematic axes and are interpreted to be coeval. Strike-slip faults form Riedel and P-shear geometries that are compatible with left-lateral slip on the Magallanes-Fagnano fault-zone. Strike-slip and normal faults occur in a releasing step-over between two overlapping left-lateral, left-stepping segments of the Magallanes fault zone and record a tectonic event defined by sinistral transtension that probably reflects changing plate dynamics associated with the opening of the Drake Passage during the Early Miocene.<br>text
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Fitch, Justin David. "Cenozoic evolution of a fragmented foreland basin, Altiplano plateau, southern Peru." 2012. http://hdl.handle.net/2152/22198.

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Debate persists on the timing, magnitude and style of crustal shortening, uplift and basin evolution in the Andes. Many studies suggest that the central Andes, including the Altiplano plateau, were gradually uplifted as a result of protracted Cenozoic retroarc shortening. However, recent isotopic studies conclude that the Andes instead rose in pulses, with the most significant event occurring at 10-6 Ma. Many researchers attribute these rapid pulses of uplift to lower lithosphere delamination events. A better understanding of the history of Cenozoic crustal shortening is essential for determination of the mechanism(s) of Andean uplift. The well-exposed Cenozoic San Jerónimo Group was studied in the Ayaviri basin of the northern Altiplano in southern Peru. The 3-5 km-thick succession is situated at 3900-4800 m elevation, between the Western Cordillera magmatic arc and the Eastern Cordillera fold-thrust-belt. New detrital zircon U-Pb geochronological results from four sandstones and one reworked tuff in the San Jerónimo succession show large age populations indicative of syndepositional volcanism between approximately 38 and 27 Ma. A 1600-m-thick magnetostratigraphic section further constrains the depositional timing and accumulation rate of the upper portion of the succession. Sedimentological observations show a rapid transition from cross-stratified braided-fluvial sandstones to proximal channel-fill and alluvial-fan conglomerates at ~30 Ma. Paleocurrent measurements show important temporal and spatial variations in sediment dispersal patterns while conglomerate clast counts show an upsection transition from almost exclusively volcanic input to increasing contributions of clastic, quartzite, and limestone detritus. The corresponding shifts in depositional environment and sediment provenance are attributed to the activation of new thrust structures in close proximity to the basin, namely the Pucapuca-Sorapata fault system, indicating the presence of an eastward advancing fold-thrust belt dating to at least 38 Ma and reaching the Ayaviri basin within the northern Altiplano plateau at ~30 Ma.<br>text
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Book chapters on the topic "Andean fold-thrust"

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Turienzo, Martín, Natalia Sánchez, Fernando Lebinson, and Luis Dimieri. "The Structure of the Southern Central Andes (Chos Malal Fold and Thrust Belt)." In The Evolution of the Chilean-Argentinean Andes. Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-67774-3_17.

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Litvak, Vanesa D., Sofía B. Iannelli, Lucía Fernández Paz, and Andrés Folguera. "The Miocene Magmatism in the Malargüe and Chos Malal Fold and Thrust Belts." In Opening and Closure of the Neuquén Basin in the Southern Andes. Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-29680-3_19.

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Acevedo, Eliana, Eduardo Agustín Rosselot, Federico Martos, Lucas Fennell, Maximiliano Naipauer, and Andrés Folguera. "Tectonic Setting of the Tordillo Formation in the Aconcagua Fold-and-Thrust Belt." In Opening and Closure of the Neuquén Basin in the Southern Andes. Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-29680-3_7.

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Bande, Alejandro, Andrés Boll, Facundo Fuentes, Brian K. Horton, and Daniel F. Stockli. "Thermochronological Constraints on the Exhumation of the Malargüe Fold-Thrust Belt, Southern Central Andes." In Opening and Closure of the Neuquén Basin in the Southern Andes. Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-29680-3_15.

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Sánchez, Natalia, Martín Turienzo, Isabelle Coutand, Fernando Lebinson, Vanesa Araujo, and Luis Dimieri. "Structural and Thermochronological Constraints on the Exhumation of the Chos Malal Fold and Thrust Belt (~37° S)." In Opening and Closure of the Neuquén Basin in the Southern Andes. Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-29680-3_13.

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A., Echaurren, Gianni Guido M., Fernández Paz Lucía, et al. "Tectonic controls on the building of the North Patagonian fold-thrust belt (~ 43°S)." In Andean Tectonics. Elsevier, 2019. http://dx.doi.org/10.1016/b978-0-12-816009-1.00022-8.

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Rojas Vera, E. A., P. Giampaoli, E. Gobbo, E. Rocha, G. Olivieri, and D. Figueroa. "Structure and tectonic evolution of the Interandean and Subandean Zones of the central Andean fold-thrust belt of Bolivia." In Andean Tectonics. Elsevier, 2019. http://dx.doi.org/10.1016/b978-0-12-816009-1.00016-2.

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Ghiglione, Matías C., Gonzalo Ronda, Rodrigo J. Suárez, et al. "Structure and tectonic evolution of the South Patagonian fold and thrust belt: Coupling between subduction dynamics, climate and tectonic deformation." In Andean Tectonics. Elsevier, 2019. http://dx.doi.org/10.1016/b978-0-12-816009-1.00024-1.

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Roeder, D., and R. L. Chamberlain. "Structural Geology of Sub-Andean Fold and Thrust Belt in Northwestern Bolivia." In Petroleum Basins of South America. American Association of Petroleum Geologists, 1995. http://dx.doi.org/10.1306/m62593c23.

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Kortyna, Cullen, Peter G. DeCelles, and Barbara Carrapa. "Structural and thermochronologic constraints on kinematics and timing of inversion of the Salta rift in the Tonco-Amblayo sector of the Andean retroarc fold-thrust belt, northwestern Argentina." In Andean Tectonics. Elsevier, 2019. http://dx.doi.org/10.1016/b978-0-12-816009-1.00018-6.

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Conference papers on the topic "Andean fold-thrust"

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Mackaman-Lofland, Chelsea, Brian K. Horton, Facundo Fuentes, et al. "KINEMATIC DEVELOPMENT AND STRUCTURAL ARCHITECTURE OF THE SOUTHERN CENTRAL ANDEAN FOLD-THRUST BELT (31−33°S): IMPLICATIONS FOR ANDEAN DEFORMATION MODES AND DRIVING MECHANISMS." In GSA Annual Meeting in Phoenix, Arizona, USA - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019am-336028.

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Anderson, Ryan Bruce, Sean P. Long, Brian K. Horton, Amanda Calle, and Victor Ramirez. "RETROARC CRUSTAL SHORTENING AND STRUCTURAL ARCHITECTURE OF THE ANDEAN FOLD-THRUST BELT OF SOUTHERN BOLIVIA (21°S): IMPLICATIONS FOR KINEMATIC DEVELOPMENT AND CRUSTAL THICKENING OF THE CENTRAL ANDES." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-284079.

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Anderson, Ryan Bruce, Sean P. Long, Brian K. Horton, Amanda Calle, and Victor Ramirez. "REGIONAL GEOLOGIC MAP ACROSS THE ANDEAN RETROARC FOLD-THRUST BELT OF SOUTHERN BOLIVIA: NEW INSIGHTS ON THE SUBANDEAN ZONE, INTERANDEAN ZONE, AND EASTERN CORDILLERA AT 21°S." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-285926.

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Mescua, José F., Laura Giambiagi, Laura Giambiagi, et al. "FEEDBACKS BETWEEN MAGMATISM AND STRESS AND STRAIN FIELDS IN THE MALARGüE FOLD AND THRUST BELT, SOUTHERN CENTRAL ANDES (34º-36ºS)." In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-302538.

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Betka, Paul, Sharon Mosher, Sharon Mosher, Keith Klepeis, and Keith Klepeis. "STRUCTURAL EVOLUTION OF THE SOUTHERN PATAGONIA RETROARC FOLD-THRUST BELT; OVER FOUR DECADES OF RESEARCH IN THE SOUTHERNMOST ANDES INSPIRED BY IAN DALZIEL." In GSA Annual Meeting in Phoenix, Arizona, USA - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019am-338405.

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