The DOI matches its Crossref record; 4 of the 4 references it cites were found in a registry or an index.
THE EVOLUTION OF THE ALTIPLANO-PUNA PLATEAU OF THE CENTRAL ANDES
Abstract
▪ Abstract The enigma of continental plateaus formed in the absence of continental collision is embodied by the Altiplano-Puna, which stretches for 1800 km along the Central Andes and attains a width of 350–400 km. The plateau correlates spatially and temporally with Andean arc magmatism, but it was uplifted primarily because of crustal thickening produced by horizontal shortening of a thermally softened lithosphere. Nonetheless, known shortening at the surface accounts for only 70–80% of the observed crustal thickening, suggesting that magmatic addition and other processes such as lithospheric thinning, upper mantle hydration, or tectonic underplating may contribute significantly to thickening. Uplift in the region of the Altiplano began around 25 Ma, coincident with increased convergence rate and inferred shallowing of subduction; uplift in the Puna commenced 5–10 million years later.
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Citations
Cites
von Huene, R., & Scholl, D. W. (1991) · Reviews of Geophysics · doi:10.1029/91rg00969 · Cited by 1,283
Uplift of the Central Andean Plateau and bending of the Bolivian Orocline
Isacks, B. L. (1988) · Journal of Geophysical Research: Solid Earth · doi:10.1029/jb093ib04p03211 · Cited by 1,113
Self-citationRelative motion of the Nazca (Farallon) and South American Plates since Late Cretaceous time
Pardo‐Casas, F., & Molnar, P. (1987) · Tectonics · doi:10.1029/tc006i003p00233 · Cited by 855
A balanced model of the southern Central Andes
Schmitz, M. (1994) · Tectonics · doi:10.1029/93tc02232 · Cited by 138
Cited by
Stern, R. J. (2002) · Reviews of Geophysics · doi:10.1029/2001rg000108 · Cited by 1,517
Andean flat-slab subduction through time
Ramos, V. A., & Folguera, A. (2009) · Geological Society, London, Special Publications · doi:10.1144/sp327.3 · Cited by 441
Orographic barriers, high-resolution TRMM rainfall, and relief variations along the eastern Andes
Bookhagen, B., & Strecker, M. R. (2008) · Geophysical Research Letters · doi:10.1029/2007gl032011 · Cited by 355
What drives orogeny in the Andes?
Sobolev, S. V., & Babeyko, A. Y. (2005) · Geology · doi:10.1130/g21557ar.1 · Cited by 354
Oncken, O., Hindle, D., Kley, J., Elger, K., Victor, P., & Schemmann, K. (2006) · Frontiers in Earth Sciences · doi:10.1007/978-3-540-48684-8_1 · Cited by 349
Metadata
- Authors
- Allmendinger, R. W., Jordan, T. E., Kay, S. M., & Isacks, B. L.
- Venue
- Annual Review of Earth and Planetary Sciences
- Publisher
- Annual Reviews
- Published
- 1997-05
- Volume
- 25
- Issue
- 1
- Pages
- 139-174
- ISSN
- 0084-6597 (ISSN-L)
- 1545-4495
- OpenAlex
- W2156642203
- Cited by
- 910
- References
- 4
- FWCI
- 7.00
- Type
- journal article
- Language
- en
- Open access
- closed
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- CoChat. (2026). Citation check: THE EVOLUTION OF THE ALTIPLANO-PUNA PLATEAU OF THE CENTRAL ANDES. https://app.cochat.ai/papers/10.1146/annurev.earth.25.1.139
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- Allmendinger, R. W., Jordan, T. E., Kay, S. M., & Isacks, B. L. (1997). THE EVOLUTION OF THE ALTIPLANO-PUNA PLATEAU OF THE CENTRAL ANDES. Annual Review of Earth and Planetary Sciences. https://doi.org/10.1146/annurev.earth.25.1.139
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Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).
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