Tectonic Evolution of the Central Andean Plateau and Implications for the Growth of Plateaus

Current end-member models for the geodynamic evolution of orogenic plateaus predict ( a ) slow and steady rise during crustal shortening and ablative subduction (i.e., continuous removal) of the lower lithosphere or ( b ) rapid surface uplift following shortening, which is associated with punctuated...

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Veröffentlicht in:Annual review of earth and planetary sciences 2017-08, Vol.45 (1), p.529-559
Hauptverfasser: Garzione, Carmala N, McQuarrie, Nadine, Perez, Nicholas D, Ehlers, Todd A, Beck, Susan L, Kar, Nandini, Eichelberger, Nathan, Chapman, Alan D, Ward, Kevin M, Ducea, Mihai N, Lease, Richard O, Poulsen, Christopher J, Wagner, Lara S, Saylor, Joel E, Zandt, George, Horton, Brian K
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container_end_page 559
container_issue 1
container_start_page 529
container_title Annual review of earth and planetary sciences
container_volume 45
creator Garzione, Carmala N
McQuarrie, Nadine
Perez, Nicholas D
Ehlers, Todd A
Beck, Susan L
Kar, Nandini
Eichelberger, Nathan
Chapman, Alan D
Ward, Kevin M
Ducea, Mihai N
Lease, Richard O
Poulsen, Christopher J
Wagner, Lara S
Saylor, Joel E
Zandt, George
Horton, Brian K
description Current end-member models for the geodynamic evolution of orogenic plateaus predict ( a ) slow and steady rise during crustal shortening and ablative subduction (i.e., continuous removal) of the lower lithosphere or ( b ) rapid surface uplift following shortening, which is associated with punctuated removal of dense lower lithosphere and or lower crustal flow. This review integrates results from recent studies of the modern lithospheric structure, geologic evolution, and surface uplift history of the Central Andean Plateau to evaluate the geodynamic processes involved in forming it. Comparison of the timing, magnitude, and distribution of shortening and surface uplift, in combination with other geologic evidence, highlights the pulsed nature of plateau growth. We discuss specific regions and time periods that show evidence for end-member geodynamic processes, including middle-late Miocene surface uplift of the southern Eastern Cordillera and Altiplano associated with shortening and ablative subduction, latest Oligocene-early Miocene and late Miocene-early Pliocene punctuated removal of dense lower lithosphere in the Eastern Cordillera and Altiplano, and late Miocene-early Pliocene crustal flow in the central and northern Altiplano.
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subjects basin evolution
crustal flow
Crustal shortening
Deformation
Geology
History
incision
Lithosphere
lower lithosphere removal
magmatism
Miocene
Oligocene
Orogeny
Plateaus
Pliocene
Removal
Subduction
Subduction (geology)
surface uplift
Uplift
title Tectonic Evolution of the Central Andean Plateau and Implications for the Growth of Plateaus
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