Fractal and Multifractal Characteristics of Lineaments in the Qianhe Graben and Its Tectonic Significance Using Remote Sensing Images

The distribution and characteristics of geological lineaments in areas with active faulting are vital for providing a basis for regional tectonic identification and analyzing the tectonic significance. Here, we extracted the lineaments in the Qianhe Graben, an active mountainous area on the southwes...

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Veröffentlicht in:Remote sensing (Basel, Switzerland) Switzerland), 2021-02, Vol.13 (4), p.587, Article 587
Hauptverfasser: Liu, Zhiheng, Han, Ling, Du, Chengyan, Cao, Hongye, Guo, Jianhua, Wang, Haiyang
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Han, Ling
Du, Chengyan
Cao, Hongye
Guo, Jianhua
Wang, Haiyang
description The distribution and characteristics of geological lineaments in areas with active faulting are vital for providing a basis for regional tectonic identification and analyzing the tectonic significance. Here, we extracted the lineaments in the Qianhe Graben, an active mountainous area on the southwest margin of Ordos Block, China, by using the tensor voting algorithm after comparing them with the segment tracing algorithm (STA) and LINE algorithm in PCI Geomatica Software. The main results show that (1) the lineaments in this area are mostly induced by the active fault events with the main trending of NW-SE, (2) the box dimensions of all lineaments, NW-SE trending lineaments, and NE-SW trending lineaments are 1.60, 1.48, and 1.44 (R-2 > 0.9), respectively, indicating that the faults exhibit statistical self-similarity, and (3) the lineaments have multifractal characteristics according to the mass index tau(q), generalized fractal dimension D(q), fractal width (Delta alpha = 2.25), fractal spectrum shape (f(alpha) is a unimodal left-hook curve), and spectrum width (Delta f = 1.21). These results are related to the tectonic activity in this area, where a higher tectonic activity leads to more lineaments being produced and a higher fractal dimension. All of these results suggest that such insights can be beneficial for providing potential targets in reconstructing the tectonic structure of the area and trends of plate movement.
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These results are related to the tectonic activity in this area, where a higher tectonic activity leads to more lineaments being produced and a higher fractal dimension. All of these results suggest that such insights can be beneficial for providing potential targets in reconstructing the tectonic structure of the area and trends of plate movement.</description><identifier>ISSN: 2072-4292</identifier><identifier>EISSN: 2072-4292</identifier><identifier>DOI: 10.3390/rs13040587</identifier><language>eng</language><publisher>BASEL: Mdpi</publisher><subject>Algorithms ; Environmental Sciences ; Environmental Sciences &amp; Ecology ; Fault lines ; fractal and multifractal characteristics ; Fractal geometry ; Fractals ; Geological faults ; Geology ; Geosciences, Multidisciplinary ; Graben ; Imaging Science &amp; Photographic Technology ; Life Sciences &amp; Biomedicine ; lineaments ; Mountain regions ; Mountainous areas ; Physical Sciences ; Qianhe Graben ; Remote Sensing ; Rivers ; Science &amp; Technology ; Self-similarity ; Technology ; tectonic significance ; Tectonics ; Tensors ; Topography ; Valleys</subject><ispartof>Remote sensing (Basel, Switzerland), 2021-02, Vol.13 (4), p.587, Article 587</ispartof><rights>2021. 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Here, we extracted the lineaments in the Qianhe Graben, an active mountainous area on the southwest margin of Ordos Block, China, by using the tensor voting algorithm after comparing them with the segment tracing algorithm (STA) and LINE algorithm in PCI Geomatica Software. The main results show that (1) the lineaments in this area are mostly induced by the active fault events with the main trending of NW-SE, (2) the box dimensions of all lineaments, NW-SE trending lineaments, and NE-SW trending lineaments are 1.60, 1.48, and 1.44 (R-2 &gt; 0.9), respectively, indicating that the faults exhibit statistical self-similarity, and (3) the lineaments have multifractal characteristics according to the mass index tau(q), generalized fractal dimension D(q), fractal width (Delta alpha = 2.25), fractal spectrum shape (f(alpha) is a unimodal left-hook curve), and spectrum width (Delta f = 1.21). These results are related to the tectonic activity in this area, where a higher tectonic activity leads to more lineaments being produced and a higher fractal dimension. All of these results suggest that such insights can be beneficial for providing potential targets in reconstructing the tectonic structure of the area and trends of plate movement.</abstract><cop>BASEL</cop><pub>Mdpi</pub><doi>10.3390/rs13040587</doi><tpages>24</tpages><orcidid>https://orcid.org/0000-0002-2794-3557</orcidid><oa>free_for_read</oa></addata></record>
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subjects Algorithms
Environmental Sciences
Environmental Sciences & Ecology
Fault lines
fractal and multifractal characteristics
Fractal geometry
Fractals
Geological faults
Geology
Geosciences, Multidisciplinary
Graben
Imaging Science & Photographic Technology
Life Sciences & Biomedicine
lineaments
Mountain regions
Mountainous areas
Physical Sciences
Qianhe Graben
Remote Sensing
Rivers
Science & Technology
Self-similarity
Technology
tectonic significance
Tectonics
Tensors
Topography
Valleys
title Fractal and Multifractal Characteristics of Lineaments in the Qianhe Graben and Its Tectonic Significance Using Remote Sensing Images
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