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Tectono-Geomorphic Analysis in Low Relief, Low Tectonic Activity Areas: Case Study of the Temiskaming Region in the Western Quebec Seismic Zone (WQSZ), Eastern Canada

Giona Bucci, Monica, Schoenbohm, Lindsay M.·2022·Remote Sensing
DOI 10.3390/rs14153587
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Abstract

We designed a workflow to investigate areas of potential neotectonic deformation, making use of well-developed techniques, but applied to a site characterized by low relief and low or moderate tectonic activity. In this pilot study, we targeted the Temiskaming Graben, in Eastern Canada, where recent and ongoing geophysical and sedimentological investigations have revealed recent activity along this ancient structure. The dataset compiled for this experimental study covers an area of nearly 147 square km across the provinces of Ontario and Quebec. For efficiency in terms of computational resources, we first performed cluster analysis on knickpoint location, identifying seven areas with a high density of disruptions along river profiles. We then performed more detailed morphometric analysis at 30 m resolution, identifying knickpoints along river profiles, calculating the hypsometric integral across the landscape with a moving window, and mapping and comparing lineaments with known structural features. The results of our workflow showed that these three techniques can be efficiently combined for neotectonic analysis, and the synergistic approach strengthens the reliability and accuracy of our results. Our research extends the application of morphometric analysis, commonly used for exploring areas with intense tectonism and high topography, to areas that are characterized by low relief and low or moderate tectonic activity. The new areas identified with the workflow proposed in this research require ground-truthing through mapping and shallow geophysical investigations.

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  • Previous research has demonstrated that a single geomorphic index is insufficient to reliably infer relative uplift rates in a vast region because uplift rates can be affected by a variety of conditions, including lithological variation which affects erosional resistance.

    “Previous research has demonstrated that a single geomorphic index is insufficient to reliably infer relative uplift rates in a vast region, such as the one studied here, because uplift rates can be affected by variety of conditions, including lithological variation which affects erosional resistance (Clayton and Shamoon 1998;Bucci and Schoenbohm 2022;Selby 1980;Telbisz et al. 2013).”

    From Tectonic geomorphology of the Ottawa-Bonnechere Graben, Eastern Canada: implications for regional uplift and intraplate seismicity (2023) · cites this paper as Bucci and Schoenbohm 2022

  • In the Timiskaming Graben, knickpoint analysis successfully identified several knickpoints coincident with previously mapped faults and lineaments.

    “For example, in the Timiskaming Graben (TG), knickpoint analysis successfully identified several knickpoints coincident with previously mapped faults and lineaments (Bucci and Schoenbohm 2022), demonstrating the power of such morphotectonic approaches.”

    From Tectonic geomorphology of the Ottawa-Bonnechere Graben, Eastern Canada: implications for regional uplift and intraplate seismicity (2023) · cites this paper as Bucci and Schoenbohm 2022

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Metadata

Authors
Giona Bucci, M., & Schoenbohm, L. M.
Affiliations
Chemical and Physical Sciences, University of Toronto at Mississauga, Mississauga, ON L5L 1C6, Canada
ORCID
Giona Bucci, Monica
Venue
Remote Sensing
Publisher
MDPI AG
Published
2022-07-26
Volume
14
Issue
15
Pages
3587
ISSN
2072-4292
DOI
10.3390/rs14153587
Cited by
11
References
0
Language
en
Licence
creativecommons.org/licenses/by/4.0/ (vor)
Funders
University of Toronto (306461)

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Statistics and arithmetic are recomputed, not judged.

Confidence bands are shown only for fields calibrated on our annotated test set. None is calibrated yet, so no band is shown.

What counts as a claim ›How we measure confidence ›How we check this ›

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