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Along-strike variations of morphotectonic features in the Western Foothills of Taiwan: tectonic implications based on stream-gradient and hypsometric analysis

Chen, Yen-Chieh, Sung, Quocheng, Cheng, Kuang-Yu·2003·Geomorphology
DOI 10.1016/s0169-555x(03)00059-x
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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 Chen et al. 2003

  • The HI profiles along the OBG present relatively constant values around 0.5, which indicates denuded topography or potentially broad-scale erosion by deglaciation.

    “The HI profiles generated along the OBG present relatively constant values of around 0.5 which indicates denuded topography (Figure 6, 7) (Strahler 1952, Kirby et al. 2003, Chen et al. 2003), or potentially broad scale erosion by deglaciation (Dyke et al. 2002).”

    From Tectonic geomorphology of the Ottawa-Bonnechere Graben, Eastern Canada: implications for regional uplift and intraplate seismicity (2023) · cites this paper as Chen et al. 2003

  • In the OBG, relative uplift rates do not correspond directly with fault slip rate, but they can provide insight into the spatial distribution and variation of relative uplift rates.

    “Although, in the OBG, the relative uplift rates does not correspond directly with fault slip rate, they can provide insight into the spatial distribution and variation of relative uplift rates”

    From Tectonic geomorphology of the Ottawa-Bonnechere Graben, Eastern Canada: implications for regional uplift and intraplate seismicity (2023) · cites this paper as Chen et al. 2003

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Metadata

Authors
Chen, Y.-C., Sung, Q., & Cheng, K.-Y.
Venue
Geomorphology
Publisher
Elsevier BV
Published
2003-11
Volume
56
Issue
1-2
Pages
109-137
ISSN
0169-555X
DOI
10.1016/s0169-555x(03)00059-x
Cited by
279
References
0
Language
en
Licence
www.elsevier.com/tdm/userlicense/1.0/ (tdm)

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