Growth of Neogene Andes linked to changes in plate convergence using high-resolution kinematic models

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Growth of Neogene Andes linked to changes in plate convergence using high-resolution kinematic models. / Quiero, Felipe; Tassara, Andres; Iaffaldano, Giampiero; Rabbia, Osvaldo.

In: Nature Communications, Vol. 13, No. 1, 1339, 2022.

Research output: Contribution to journalJournal articleResearchpeer-review

Harvard

Quiero, F, Tassara, A, Iaffaldano, G & Rabbia, O 2022, 'Growth of Neogene Andes linked to changes in plate convergence using high-resolution kinematic models', Nature Communications, vol. 13, no. 1, 1339. https://doi.org/10.1038/s41467-022-29055-4

APA

Quiero, F., Tassara, A., Iaffaldano, G., & Rabbia, O. (2022). Growth of Neogene Andes linked to changes in plate convergence using high-resolution kinematic models. Nature Communications, 13(1), [1339]. https://doi.org/10.1038/s41467-022-29055-4

Vancouver

Quiero F, Tassara A, Iaffaldano G, Rabbia O. Growth of Neogene Andes linked to changes in plate convergence using high-resolution kinematic models. Nature Communications. 2022;13(1). 1339. https://doi.org/10.1038/s41467-022-29055-4

Author

Quiero, Felipe ; Tassara, Andres ; Iaffaldano, Giampiero ; Rabbia, Osvaldo. / Growth of Neogene Andes linked to changes in plate convergence using high-resolution kinematic models. In: Nature Communications. 2022 ; Vol. 13, No. 1.

Bibtex

@article{0dfe6acccf154b76a2a64b310a5245f5,
title = "Growth of Neogene Andes linked to changes in plate convergence using high-resolution kinematic models",
abstract = "The Andean cordillera was constructed during compressive tectonic events, whose causes and controls remain unclear. Exploring a possible link to plate convergence has been impeded by the coarse temporal resolution of existing plate kinematic models. Here we show that the Neogene evolution of the Andean margin is primarily related to changes in convergence as observed in new high-resolution plate reconstructions. Building on a compilation of plate finite rotations spanning the last 30 million years and using noise-mitigation techniques, we predict several short-term convergence changes that were unresolved in previous models. These changes are related to main tectono-magmatic events and require forces that are compatible with a range of geodynamic processes. These results allow to revise models of ongoing subduction orogeny at its type locality, emphasizing the role of upper plate deformation in the balance between kinematic energy associated with plate motion and gravitational potential energy stored in orogenic crustal roots.",
author = "Felipe Quiero and Andres Tassara and Giampiero Iaffaldano and Osvaldo Rabbia",
note = "Publisher Copyright: {\textcopyright} 2022, The Author(s).",
year = "2022",
doi = "10.1038/s41467-022-29055-4",
language = "English",
volume = "13",
journal = "Nature Communications",
issn = "2041-1723",
publisher = "nature publishing group",
number = "1",

}

RIS

TY - JOUR

T1 - Growth of Neogene Andes linked to changes in plate convergence using high-resolution kinematic models

AU - Quiero, Felipe

AU - Tassara, Andres

AU - Iaffaldano, Giampiero

AU - Rabbia, Osvaldo

N1 - Publisher Copyright: © 2022, The Author(s).

PY - 2022

Y1 - 2022

N2 - The Andean cordillera was constructed during compressive tectonic events, whose causes and controls remain unclear. Exploring a possible link to plate convergence has been impeded by the coarse temporal resolution of existing plate kinematic models. Here we show that the Neogene evolution of the Andean margin is primarily related to changes in convergence as observed in new high-resolution plate reconstructions. Building on a compilation of plate finite rotations spanning the last 30 million years and using noise-mitigation techniques, we predict several short-term convergence changes that were unresolved in previous models. These changes are related to main tectono-magmatic events and require forces that are compatible with a range of geodynamic processes. These results allow to revise models of ongoing subduction orogeny at its type locality, emphasizing the role of upper plate deformation in the balance between kinematic energy associated with plate motion and gravitational potential energy stored in orogenic crustal roots.

AB - The Andean cordillera was constructed during compressive tectonic events, whose causes and controls remain unclear. Exploring a possible link to plate convergence has been impeded by the coarse temporal resolution of existing plate kinematic models. Here we show that the Neogene evolution of the Andean margin is primarily related to changes in convergence as observed in new high-resolution plate reconstructions. Building on a compilation of plate finite rotations spanning the last 30 million years and using noise-mitigation techniques, we predict several short-term convergence changes that were unresolved in previous models. These changes are related to main tectono-magmatic events and require forces that are compatible with a range of geodynamic processes. These results allow to revise models of ongoing subduction orogeny at its type locality, emphasizing the role of upper plate deformation in the balance between kinematic energy associated with plate motion and gravitational potential energy stored in orogenic crustal roots.

U2 - 10.1038/s41467-022-29055-4

DO - 10.1038/s41467-022-29055-4

M3 - Journal article

C2 - 35292661

AN - SCOPUS:85126696178

VL - 13

JO - Nature Communications

JF - Nature Communications

SN - 2041-1723

IS - 1

M1 - 1339

ER -

ID: 310835909