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Quantifying rock uplift rates using channel steepness and cosmogenic nuclide–determined erosion rates: Examples from northern and southern Italy

Cyr, Andrew J., Granger, Darryl E., Olivetti, Valerio, Molin, Paola·2010·Lithosphere
DOI 10.1130/l96.1
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  • Morphotectonic analysis integrating multiple geomorphic indices has been used successfully to identify relative tectonic uplift rate associated with present-day seismicity and regional stress in various tectonic settings.

    “Morphotectonic analysis which integrates multiple geomorphic indices, has been used successfully to identify the relative tectonic uplift rate associated with the present-day seismicity and regional stress in various tectonic settings (compressional, extensional, and strikeslip/oblique-slip) (Chen et al. 2003;Cyr et al. 2010;El Hamdouni et al. 2008;Krystopowicz et al. 2020;Rimando and Schoenbohm 2”

    From Tectonic geomorphology of the Ottawa-Bonnechere Graben, Eastern Canada: implications for regional uplift and intraplate seismicity (2023) · cites this paper as Cyr et al. 2010

  • To better characterize spatial distribution of relative uplift rate using ksn values, several parameters should be considered that may contribute to uplift rate variation such as lithologic contrast, precipitation rate, and stream capture.

    “Therefore, to better characterize spatial distribution of relative uplift rate using k sn values several parameters should be considered that may contribute to uplift rate variation such as lithologic contrast (Cyr et al. 2010;Duvall 2004;Hack 1973), precipitation rate (e.g., (Bookhagen and Strecker 2012), and stream capture (Robl et al. 2017).”

    From Tectonic geomorphology of the Ottawa-Bonnechere Graben, Eastern Canada: implications for regional uplift and intraplate seismicity (2023) · cites this paper as Cyr et al. 2010

  • In various tectonic and geologic settings with variable climatic regimes and rock types, a linear relationship between ksn and uplift rate has been demonstrated.

    “In various tectonic and geologic settings with variable climatic regimes and rock types, a linear relationship between k sn and uplift rate has been demonstrated (Snyder et al. 2000, Wobus et al. 2006, Cyr et al. 2010, DiBiase et al. 2010, Kirby and Whipple 2012).”

    From Tectonic geomorphology of the Ottawa-Bonnechere Graben, Eastern Canada: implications for regional uplift and intraplate seismicity (2023) · cites this paper as Cyr et al. 2010

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Metadata

Authors
Cyr, A. J., Granger, D. E., Olivetti, V., & Molin, P.
Venue
Lithosphere
Publisher
GeoScienceWorld
Published
2010-06
Volume
2
Issue
3
Pages
188-198
ISSN
  • 1947-4253
  • 1941-8264
DOI
10.1130/l96.1
Cited by
191
References
0
Language
en

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