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Dynamic Topography Using Remote Sensing: Multidisciplinary Approaches to Detect and Model Earth’s Surface Processes

A special issue of Remote Sensing (ISSN 2072-4292). This special issue belongs to the section "Remote Sensing in Geology, Geomorphology and Hydrology".

Deadline for manuscript submissions: closed (31 March 2025) | Viewed by 1903

Special Issue Editors


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Guest Editor
Department of Geophysics and Space Sciences, Eötvös Loránd University, 1117 Budapest, Hungary
Interests: slope; digital terrain analysis; landslide; remote sensing
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Guest Editor
Department of the Geological Survey of Italy, Italian Institute for Environmental Protection and Research (ISPRA), 00144 Rome, Italy
Interests: geomorphology; natural hazards; neotectonics; landslides; geological mapping
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Department of Environmental Sciences, Informatics and Statistics, Ca’ Foscari University of Venice, 30170 Mestre, Italy
Interests: geomorphology; active tectonic; geochronology; coastal dynamic
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Guest Editor
Department of Earth Sciences, Sapienza University of Rome, P.le A. Moro 5, 00185 Rome, Italy
Interests: landslides; fluvial geomorphology; terrain analysis; landscape evolution modelling
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Guest Editor
Department of Earth Sciences, University of Florence, 50121 Florence, Italy
Interests: structural geology; geomorphology; mountain building dynamics; fault mechanics

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Guest Editor
Department of Earth and Environmental Sciences, Lehigh University, Bethlehem, PA 18015, USA
Interests: geomorphology; active tectonics; geology

Special Issue Information

Dear Colleagues,

Surface responses to allogenic forcings (climate and tectonic) and autogenic processes occurring at different time scales (days to millennials) and frequencies (periodic to quasi-periodic) modulate the spatio-temporal distribution of local-to-global scale environmental changes. Remote sensing provides snapshots of this evolution and act as a crucial support in both classical and new techniques of Earth’s surface observation and change detection (field-based survey, geochronology, LEM, machine learning, DInSAR, etc.), which allows us to understand how geological, climate, and even anthropogenic events control each other at various time scales. GPS, UAV, satellite images, and laser scanning are extensively used to understand earthquake mechanics (i.e., co-seismic slip), landmass failures hazard, fluvio-deltaic depositional dynamics, fluvial and slope erosional cycles, vegetation cover and land use evolution, sediments provenance and routing, etc.

In this Special Issue, we aim to focus on multidisciplinary studies that apply remote sensing techniques and explore spatio-temporal surface evolution in response to different forcings and processes, such as crustal deformation and fluvial reorganization, as well as investigate the impact of climate change on surface processes and anthropic spreading. We also invite submissions that combine remote sensing with other classical and innovative approaches, focusing on modelling regional geomorphic evolution, rock type detection, natural hazard assessments, strain partitioning in tectonically active region, erosional-depositional dynamics, etc.

Potential topics include, but not limited to, the following:

  • Tectonic processes;
  • Climate change-related surface evolution;
  • Drainage systems reorganization;
  • Fault slip detection, strain partitioning and seismic cycles;
  • Fluvial-deltaic sediments’ evolution, routing and deposition;
  • Geomorphology and land use changes.

Dr. Balázs Székely
Dr. Mauro Bonasera
Dr. Ciro Cerrone
Dr. Michele Delchiaro
Dr. Riccardo Lanari
Dr. Francesco Pavano
Guest Editors

Manuscript Submission Information

Manuscripts should be submitted online at www.mdpi.com by registering and logging in to this website. Once you are registered, click here to go to the submission form. Manuscripts can be submitted until the deadline. All submissions that pass pre-check are peer-reviewed. Accepted papers will be published continuously in the journal (as soon as accepted) and will be listed together on the special issue website. Research articles, review articles as well as short communications are invited. For planned papers, a title and short abstract (about 100 words) can be sent to the Editorial Office for announcement on this website.

Submitted manuscripts should not have been published previously, nor be under consideration for publication elsewhere (except conference proceedings papers). All manuscripts are thoroughly refereed through a single-blind peer-review process. A guide for authors and other relevant information for submission of manuscripts is available on the Instructions for Authors page. Remote Sensing is an international peer-reviewed open access semimonthly journal published by MDPI.

Please visit the Instructions for Authors page before submitting a manuscript. The Article Processing Charge (APC) for publication in this open access journal is 2700 CHF (Swiss Francs). Submitted papers should be well formatted and use good English. Authors may use MDPI's English editing service prior to publication or during author revisions.

Keywords

  • tectonic deformation
  • earthquake ground deformation
  • landslides
  • fluvial-deltaic dynamics
  • sediments routing
  • source-to-sink analysis

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Published Papers (1 paper)

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Research

17 pages, 14394 KiB  
Article
Quaternary Deformation along the Gobi–Tian Shan Fault in the Easternmost Tian Shan (Harlik Mountain), Central Asia
by Tianyi Shen, Yan Ding, Guocan Wang, Dehai Zhang and Zihao Zhao
Remote Sens. 2024, 16(17), 3343; https://doi.org/10.3390/rs16173343 - 9 Sep 2024
Viewed by 1201
Abstract
The Tian Shan is a typical active intracontinental orogenic belt that is driven by the ongoing indentation of India into Eurasia. However, the geological features of Quaternary deformation, especially in the easternmost sector near Harlik Mountain, remain elusive. Field observations, topographic analysis, and [...] Read more.
The Tian Shan is a typical active intracontinental orogenic belt that is driven by the ongoing indentation of India into Eurasia. However, the geological features of Quaternary deformation, especially in the easternmost sector near Harlik Mountain, remain elusive. Field observations, topographic analysis, and Electron Spin Resonance (ESR) dating were employed to comprehensively assess the deformation features and evaluate the deformation pattern for this region during the Quaternary period. The results disclose evidence of deformation in the northern and southern foreland basins of Harlik Mountain. In the Barkol Basin to the north, crustal shortening results in the formation of surface scarps and folds, indicating north-directed thrusting, with a shortening rate of ~0.15 mm/yr. In the Hami Basin, the north-directed thrust elevates the granites, which offset the alluvial fans, with a shortening rate of ~0.18 mm/yr. Together with the shortening along the boundary fault, the aggregated north–south shortening rate is approximately 0.69 mm/yr in the easternmost Tian Shan, corresponding with the differential motion rate between the north and south Harlik Mountain revealed by the GPS velocity. These findings imply that, distal to the collision zone, tectonic strain in the eastern Tian Shan is primarily accommodated through the reactivation of pre-existing strike–slip faults, with crustal shortening concentrated at the overlapping position of parallel northeast-trending left-lateral strike–slip faults. Full article
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