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Surface uplift in the Central Andes driven by growth of the Altiplano Puna Magma Body

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  • Jonathan P. Perkins

    (University of California Santa Cruz
    Present address: U.S. Geological Survey, 345 Middlefield Road, Menlo Park, California 94025, USA)

  • Kevin M. Ward

    (The University of Arizona)

  • Shanaka L. de Silva

    (College of Earth, Ocean, and Atmospheric Sciences, Oregon State University)

  • George Zandt

    (The University of Arizona)

  • Susan L. Beck

    (The University of Arizona)

  • Noah J. Finnegan

    (University of California Santa Cruz)

Abstract

The Altiplano-Puna Magma Body (APMB) in the Central Andes is the largest imaged magma reservoir on Earth, and is located within the second highest orogenic plateau on Earth, the Altiplano-Puna. Although the APMB is a first-order geologic feature similar to the Sierra Nevada batholith, its role in the surface uplift history of the Central Andes remains uncertain. Here we show that a long-wavelength topographic dome overlies the seismically measured extent of the APMB, and gravity data suggest that the uplift is isostatically compensated. Isostatic modelling of the magmatic contribution to dome growth yields melt volumes comparable to those estimated from tomography, and suggests that the APMB growth rate exceeds the peak Cretaceous magmatic flare-up in the Sierran batholith. Our analysis reveals that magmatic addition may provide a contribution to surface uplift on par with lithospheric removal, and illustrates that surface topography may help constrain the magnitude of pluton-scale melt production.

Suggested Citation

  • Jonathan P. Perkins & Kevin M. Ward & Shanaka L. de Silva & George Zandt & Susan L. Beck & Noah J. Finnegan, 2016. "Surface uplift in the Central Andes driven by growth of the Altiplano Puna Magma Body," Nature Communications, Nature, vol. 7(1), pages 1-10, December.
  • Handle: RePEc:nat:natcom:v:7:y:2016:i:1:d:10.1038_ncomms13185
    DOI: 10.1038/ncomms13185
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    Cited by:

    1. Zhipeng Zhou & Hans Thybo & Irina M. Artemieva & Timothy Kusky & Chi-Chia Tang, 2024. "Crustal melting and continent uplift by mafic underplating at convergent boundaries," Nature Communications, Nature, vol. 15(1), pages 1-9, December.

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