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Geodynamics of a Cordilleran
Orogenic System
The Central Andes of
Argentina and Northern Chile
Edited by
Peter G. DeCelles, Mihai N. Ducea, Barbara Carrapa, and Paul A. Kapp
Geodynamics of a This memoir brings together results from a six-year,
Cordilleran Orogenic System multidisciplinary study of the linkages among processes
that have formed the highest, widest part of the Andean
The Central Andes of Cordilleran orogenic belt in northern Argentina and
Argentina and Northern Chile Chile. The region features a tectonically erosive forearc,
protracted arc magmatism, a high-elevation hinterland
Edited by Peter G. DeCelles, Mihai N. Ducea, plateau and strongly shortened retroarc thrust belt, and a
Barbara Carrapa, and Paul A. Kapp Paleocene–Recent foreland basin system. Surface geology
records spatially complex shortening, extension, mafic
Me$m6be3r.P0ri0ce to felsic magmatism, hinterland basin development,
elevation change, and regional foreland basin migration.
Memoir 212 Seismological and geodynamic studies demonstrate a
complex, dynamic upper mantle marked by widespread
foundering of dense lithosphere formed by magmatic and
metamorphic processes beneath the hinterland. Diverse
processes operating over the past 60 m.y. in the central
Andes define a tectono-magmatic cycle with a periodicity
of ca. 25–30 m.y., providing a new framework for
interpreting Cordilleran orogenic systems worldwide.
MWR212, 490 p., ISBN 9780813712123
$90.00, member price $63.00
Memoir 212 toll-free 1.888.443.4472
1.303.357.1000, option 3
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