South-American plate advance and forced Andean trench retreat as drivers for transient flat subduction episodes

scientific article published on 16 May 2017

South-American plate advance and forced Andean trench retreat as drivers for transient flat subduction episodes is …
instance of (P31):
scholarly articleQ13442814

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P819ADS bibcode2017NatCo...815249S
P356DOI10.1038/NCOMMS15249
P932PMC publication ID5440808
P698PubMed publication ID28508893

P50authorNadine McQuarrieQ61144671
Lydian M. BoschmanQ61160170
Wim SpakmanQ92369817
Douwe van HinsbergenQ98843030
P2093author name stringGerben Schepers
Martha E Kosters
P2860cites workThe role of ridges in the formation and longevity of flat slabsQ34489253
Reconciling surface plate motions with rapid three-dimensional mantle flow around a slab edgeQ46877748
Absolute plate motions in a reference frame defined by moving hot spots in the Pacific, Atlantic, and Indian oceansQ100556795
Towards absolute plate motions constrained by lower-mantle slab remnantsQ100556822
Active Andean volcanism: its geologic and tectonic settingQ51602246
Evolution and diversity of subduction zones controlled by slab width.Q55043602
Global continental and ocean basin reconstructions since 200MaQ55877778
Geodynamics of flat subduction: Seismicity and tomographic constraints from the Andean marginQ56032384
Kinematic reconstruction of the Caribbean region since the Early JurassicQ56057534
Kinematics of subduction and subduction-induced flow in the upper mantleQ56771334
On the uncertainties in hot spot reconstructions and the significance of moving hot spot reference framesQ57406273
Three-dimensional numerical models of the influence of a buoyant oceanic plateau on subduction zonesQ57525895
Seismic anisotropy around subduction zones: Insights from three-dimensional modeling of upper mantle deformation and SKS splitting calculationsQ57866355
Chilean flat slab subduction controlled by overriding plate thickness and trench rollbackQ58080167
Subduction system and flat slab beneath the Eastern Cordillera of ColombiaQ58457778
Andean flat-slab subduction through timeQ59248107
Spatial distribution of earthquakes and subduction of the Nazca plate beneath South AmericaQ59263027
Overriding plate, mantle wedge, slab, and subslab contributions to seismic anisotropy beneath the northern Central Andean PlateauQ59787422
Cyclicity in Cordilleran orogenic systemsQ59794544
Effects of change in slab geometry on the mantle flow and slab fabric in Southern PeruQ60708611
Imaging the transition from flat to normal subduction: variations in the structure of the Nazca slab and upper mantle under southern Peru and northwestern BoliviaQ60708615
Slab1.0: A three-dimensional model of global subduction zone geometriesQ60957858
Global plate motion frames: Toward a unified modelQ64357446
Tectonic shortening and crustal thickness in the Central Andes: How good is the correlation?Q67222573
Trench-parallel flow beneath the nazca plate from seismic anisotropyQ81182361
The lack of correlation between flat slabs and bathymetric impactors in South AmericaQ97744073
Kinematic reconstruction of the Bolivian oroclineQ98177718
Thermo-mechanical controls of flat subduction: Insights from numerical modelingQ98284538
P275copyright licenseCreative Commons Attribution 4.0 InternationalQ20007257
P6216copyright statuscopyrightedQ50423863
P407language of work or nameEnglishQ1860
P304page(s)15249
P577publication date2017-05-16
P1433published inNature CommunicationsQ573880
P1476titleSouth-American plate advance and forced Andean trench retreat as drivers for transient flat subduction episodes
P478volume8

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cites work (P2860)
Q47113299Andean mountain building and magmatic arc migration driven by subduction-induced whole mantle flow.
Q60122646Midcrustal Deformation in the Central Andes Constrained by Radial Anisotropy
Q97446978Reconstruction of Subduction and Back‐Arc Spreading in the NW Pacific and Aleutian Basin: Clues to Causes of Cretaceous and Eocene Plate Reorganizations
Q61013193Southward propagation of Nazca subduction along the Andes
Q97446986The Dynamic History of 220 Million Years of Subduction Below Mexico: A Correlation Between Slab Geometry and Overriding Plate Deformation Based on Geology, Paleomagnetism, and Seismic Tomography

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