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Measurement of tectonic surface uplift rate in a young collisional mountain belt

Author

Listed:
  • Lon D. Abbott

    (University of California
    Down To Earth Technology)

  • Eli A. Silver

    (University of California)

  • Robert S. Anderson

    (University of California)

  • Randall Smith

    (Geolnformation Technology)

  • James C. Ingle

    (Stanford University)

  • Stanley A. Kling
  • David Haig

    (University of Western Australia)

  • Eric Small

    (University of California)

  • Joseph Galewsky

    (University of California)

  • William S. Sliter

    (Western Geologic Mapping Team-Mail Stop 975)

Abstract

Measurement of the rate of tectonically driven surface uplift is crucial to a complete understanding of mountain building dynamics. The lack of a suitable rock record typically prevents determination of this quantity, but the unusual geology of Papua New Guinea's Finisterre mountains makes measurement of this rate possible. The tectonic surface uplift rate at the Finisterre range is 0.8-2.1 mmyr-1, approximately that expected to arise from crustal thickening.

Suggested Citation

  • Lon D. Abbott & Eli A. Silver & Robert S. Anderson & Randall Smith & James C. Ingle & Stanley A. Kling & David Haig & Eric Small & Joseph Galewsky & William S. Sliter, 1997. "Measurement of tectonic surface uplift rate in a young collisional mountain belt," Nature, Nature, vol. 385(6616), pages 501-507, February.
    • Handle: RePEc:nat:nature:v:385:y:1997:i:6616:d:10.1038_385501a0
    DOI: 10.1038/385501a0
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