Vertical GPS ground motion rates in the Euro‐Mediterranean region: New evidence of velocity gradients at different spatial scales along the Nubia‐Eurasia plate boundary
Abstract
We use 2.5 to 14 years long position time series from >800 continuous Global Positioning System (GPS) stations to study vertical deformation rates in the Euro‐Mediterranean region. We estimate and remove common mode errors in position time series using a principal component analysis, obtaining a significant gain in the signal‐to‐noise ratio of the displacements data. Following the results of a maximum likelihood estimation analysis, which gives a mean spectral index ~ −0.7, we adopt a power law + white noise stochastic model in estimating the final vertical rates and find 95% of the velocities within ±2 mm/yr, with uncertainties from filtered time series ~40% smaller than from the unfiltered ones. We highlight the presence of statistically significant velocity gradients where the stations density is higher. We find undulations of the vertical velocity field at different spatial scales both in tectonically active regions, like eastern Alps, Apennines, and eastern Mediterranean, and in regions characterized by a low or negligible tectonic activity, like central Iberia and western Alps. A correlation between smooth vertical velocities and topographic features is apparent in many sectors of the study area. Glacial isostatic adjustment and weathering processes do not completely explain the measured rates, and a combination of active tectonics and deep‐seated geodynamic processes must be invoked. Excluding areas where localized processes are likely, or where subduction processes may be active, mantle dynamics is the most likely process, but regional mantle modeling is required for a better understanding.
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The inferred maximum post-LIA uplift rate of up to a few mm yr-1 from experiments with or without a low asthenospheric thermal anomaly (TA ≤ 100 °C) is within the same order of magnitude of maximum uplift rates measured in collisional orogens such as the European Alps and the Himalayas.
“The inferred maximum post-LIA uplift rate of up to a few mm yr -1 from experiments with or without a low asthenospheric thermal anomaly (TA ≤ 100 °C, Fig. 7c) is within the same order of magnitude of maximum uplift rates measured in collisional orogens such as the European Alps”
From Fast uplift in the southern Patagonian Andes due to long- and short-term deglaciation and the asthenospheric window underneath (2024) · cites this paper as Serpelloni et al., 2013
Section 6.2 (p. 15) reports measured Alpine uplift of about 1–2 mm/yr, with central Alpine rates exceeding 2 mm/yr. That supports the same-order-of-magnitude comparison for the European Alps. The supplied claim also names the Himalayas, but the cited paper’s passages do not establish Himalayan uplift rates; the post-LIA experiments are the citing authors’ own context. (LLM, conf=0.83)
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- Authors
- Serpelloni, E., Faccenna, C., Spada, G., Dong, D., & Williams, S. D. P.
- Affiliations
- Istituto Nazionale di Geofisica e Vulcanologia (IT)
- Roma Tre University (IT)
- University of Urbino (IT)
- East China Normal University (CN)
- National Oceanography Centre Liverpool UK
- Venue
- Journal of Geophysical Research: Solid Earth
- Publisher
- American Geophysical Union (AGU)
- Published
- 2013-11
- Volume
- 118
- Issue
- 11
- Pages
- 6003-6024
- ISSN
- 2169-9313 (ISSN-L)
- 2169-9356
- OpenAlex
- W1531843072
- Cited by
- 350
- References
- 132
- Citations by year
- 2026: 11 · 2025: 15 · 2024: 39 · 2023: 25 · 2022: 29 · 2021: 36 · 2020: 44 · 2019: 27 · 2018: 37 · 2017: 19 · 2016: 28 · 2015: 22 · 2014: 17
- FWCI
- 22.21
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Journal of Geophysical Research Solid Earth (publishedVersion)
- NERC Open Research Archive (Natural Environment Research Council) (acceptedVersion)
- Archivio istituzionale della ricerca (Alma Mater Studiorum Università di Bologna) (submittedVersion)
- Iris (Roma Tre University) (submittedVersion)
- CINECA IRIS Institutional Research information system (University of Urbino) (submittedVersion)
- Funders
- Ministero dell’Istruzione, dell’Università e della Ricerca
- University of Crete
- Istituto Nazionale di Geofisica e Vulcanologia
- University of California, San Diego
- Natural Environment Research Council (noc010012, BIGF010001)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Geophysics › earthquake and tectonic studies
- Physical Sciences › Engineering › Aerospace Engineering › GNSS positioning and interference
- Physical Sciences › Earth and Planetary Sciences › Geophysics › Geological and Geophysical Studies Worldwide
- Keywords
- vertical velocity gradient, Euro-Mediterranean region, GPS time series, principal component analysis, glacial isostatic adjustment, weathering, mantle dynamics, active tectonics, Eastern Alps, Apennines, Eastern Mediterranean, Western Alps, Iberia
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