remotesensing-logo

Journal Browser

Journal Browser

Ground Deformation Patterns Detection by InSAR and GNSS Techniques (3rd Edition)

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: 28 September 2025 | Viewed by 341

Special Issue Editors


E-Mail Website
Guest Editor

E-Mail Website
Guest Editor Assistant
Department of Earth and Marine Sciences, University of Palermo, Via Archirafi 22, 90123 Palermo, Italy
Interests: near-surface geophysics; ERT; SRT; GPR; geodetic monitoring and modeling

E-Mail Website
Guest Editor Assistant
Istituto Nazionale di Geofisica e Vulcanologia, Osservatorio Etneo—Sezione di Catania, 95125 Catania, Italy
Interests: GNSS; geodynamics; volcano geodesy; land subsidence; modeling

Special Issue Information

Dear Colleagues,

The rapid development of multi-GNSS constellations (GPS, GLONASS, BDS and Galileo) and improvements in InSAR imaging allows for the acquisition of both continuous and spatially extensive datasets over large regions of the Earth. These datasets are able to capture, with high resolution, the deformations occurring at various spatial and temporal scales, therefore providing important constraints on ongoing crustal processes. Most of these datasets are used on a large scale to provide strong constraints of the motion of plates and crustal blocks. Moreover, these datasets are also used to study pre-eruptive inflation, dike intrusion and co-eruptive deflation on active volcanoes, as well as the co- and post-seismic deformation fields related to large earthquakes and the detection of subsidence associated with the extraction of mineral resources from the subsoil. Novel techniques such as GNSS reflectometry have shown a high potential to provide valuable information on ocean, land, or the cryosphere. Advanced InSAR processing techniques are currently enabling the production of high-quality maps of wide areas characterized by rapid changes such as the ones damaged by earthquakes, fires, floods, etc.

This Special Issue aims to provide a complete state-of-the-art description of all the topics mentioned above. Review contributions as well as papers describing new measurement concepts/sensors are welcomed.

Prof. Dr. Mimmo Palano
Guest Editor

Dr. Alessandra Carollo
Dr. Federica Sparacino
Guest Editor Assistants

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

  • earthquakes
  • plate motion
  • volcano geodesy
  • land subsidence
  • GNSS reflectometry
  • ground deformation modelling

Benefits of Publishing in a Special Issue

  • Ease of navigation: Grouping papers by topic helps scholars navigate broad scope journals more efficiently.
  • Greater discoverability: Special Issues support the reach and impact of scientific research. Articles in Special Issues are more discoverable and cited more frequently.
  • Expansion of research network: Special Issues facilitate connections among authors, fostering scientific collaborations.
  • External promotion: Articles in Special Issues are often promoted through the journal's social media, increasing their visibility.
  • e-Book format: Special Issues with more than 10 articles can be published as dedicated e-books, ensuring wide and rapid dissemination.

Further information on MDPI's Special Issue policies can be found here.

Related Special Issue

Published Papers (1 paper)

Order results
Result details
Select all
Export citation of selected articles as:

Other

15 pages, 3313 KiB  
Technical Note
Early Post-Seismic Deformation Revealed After the Wushi (China) Earthquake (Mw = 7.1) Occurred on 22 January 2024
by Xiaoran Lv, Guichun Luo, Lifu Zheng, Bozhi Zhang and Chen Zhang
Remote Sens. 2025, 17(8), 1340; https://doi.org/10.3390/rs17081340 - 9 Apr 2025
Viewed by 260
Abstract
The Mw = 7.1 Wushi earthquake is the second-largest digitally recorded earthquake in the Tianshan seismic zone and provides an opportunity to explore the structural characteristics of the Tianshan seismic zone. In this study, we calculated the early (11-month) post-seismic deformation of the [...] Read more.
The Mw = 7.1 Wushi earthquake is the second-largest digitally recorded earthquake in the Tianshan seismic zone and provides an opportunity to explore the structural characteristics of the Tianshan seismic zone. In this study, we calculated the early (11-month) post-seismic deformation of the Wushi earthquake using Sentine-1 ascending and descending InSAR time series data. We found that the 11-month post-seismic deformation was dominated by afterslip along the up-dip continuation of the coseismic fault. The seismic moment released by the afterslip was Mw = 6.20, with 6.5% of that released by the mainshock. Moreover, we explored four slip models for the Mw = 5.7 aftershock that occurred on 29 January and found that this event primarily ruptured a thrust fault. However, determining the thrust fault type based on the current field investigations and InSAR data remains difficult. Finally, the Coulomb stress changes indicated that both the afterslip and aftershock were promoted by the Wushi earthquake. Full article
Show Figures

Figure 1

Back to TopTop