{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2026,2,26]],"date-time":"2026-02-26T01:50:33Z","timestamp":1772070633299,"version":"3.50.1"},"reference-count":65,"publisher":"MDPI AG","issue":"10","license":[{"start":{"date-parts":[[2018,10,10]],"date-time":"2018-10-10T00:00:00Z","timestamp":1539129600000},"content-version":"vor","delay-in-days":0,"URL":"https:\/\/creativecommons.org\/licenses\/by\/4.0\/"}],"content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":["Remote Sensing"],"abstract":"<jats:p>In order to make inferences on the geodynamics of Antarctica, geodetic and gravimetric maps derived from past and new observations can be used. This paper provides new insights into the geodynamics of Antarctica by integrating data at regional and continental scales. In particular, signatures of geodynamic activity at a regional extent have been investigated in Victoria Land (VL, Antarctica) by means of Global Navigation Satellite System (GNSS) permanent station observations, data from the VLNDEF (Victoria Land Network for Deformation control) discontinuous network, and gravity station measurements. At the continental scale, episodic GNSS observations on VLNDEF sites collected for 20 years, together with continuous data from the International GNSS Service (IGS) and Polar Earth Observing Network (POLENET) sites, were processed, and the Euler pole position assessed with the angular velocity of the Antarctic plate. Both the Bouguer and the free-air gravity anomaly maps were obtained by integrating the available open-access geophysics dataset, and a compilation of 180 gravity measurements collected in the VL within the Italian National Program for Antarctic Research (PNRA) activities. As a result, new evidence has been detected at regional and continental scale. The main absolute motion of VL is towards SE (Ve 9.9 \u00b1 0.26 mm\/yr, Vn \u221211.9 \u00b1 0.27 mm\/yr) with a pattern similar to the transforms of the Tasman and Balleny fracture zones produced as consequence of Southern Ocean spreading. Residual velocities of the GNSS stations located in VL confirm the active role of the two main tectonic lineaments of the region, the Rennick\u2013Aviator and the Lillie\u2013Tucker faults with right-lateral sense of shear. The resulting VL gravity anomalies show a NW region characterized by small sized Bouguer anomaly with high uplift rates associated and a SE region with low values of Bouguer anomaly and general subsidence phenomena. The East and West Antarctica are characterized by a different thickness of the Earth\u2019s crust, and the relative velocities obtained by the observed GNSS data confirm that movements between the two regions are negligible. In East Antarctica, the roots of the main subglacial highlands, Gamburtsev Mts and Dronning Maud Land, are present. The Northern Victoria Land (NVL) is characterized by more scattered anomalies. These confirm the differences between the Glacial Isostatic Adjustment (GIA) modeled and observed uplift rates that could be related to deep-seated, regional scale structures.<\/jats:p>","DOI":"10.3390\/rs10101608","type":"journal-article","created":{"date-parts":[[2018,10,10]],"date-time":"2018-10-10T11:53:13Z","timestamp":1539172393000},"page":"1608","update-policy":"https:\/\/doi.org\/10.3390\/mdpi_crossmark_policy","source":"Crossref","is-referenced-by-count":18,"title":["New Geodetic and Gravimetric Maps to Infer Geodynamics of Antarctica with Insights on Victoria Land"],"prefix":"10.3390","volume":"10","author":[{"given":"Antonio","family":"Zanutta","sequence":"first","affiliation":[{"name":"Dipartimento di Ingegneria Civile, Chimica, Ambientale e dei Materiali\u2014Universit\u00e0 di Bologna, 40136 Bologna, Italy"}]},{"ORCID":"https:\/\/orcid.org\/0000-0002-0064-5533","authenticated-orcid":false,"given":"Monia","family":"Negusini","sequence":"additional","affiliation":[{"name":"Istituto di Radioastronomia\u2014Istituto Nazionale di Astrofisica, 40129 Bologna, Italy"}]},{"ORCID":"https:\/\/orcid.org\/0000-0002-9815-1004","authenticated-orcid":false,"given":"Luca","family":"Vittuari","sequence":"additional","affiliation":[{"name":"Dipartimento di Ingegneria Civile, Chimica, Ambientale e dei Materiali\u2014Universit\u00e0 di Bologna, 40136 Bologna, Italy"}]},{"given":"Leonardo","family":"Martelli","sequence":"additional","affiliation":[{"name":"Dipartimento di Ingegneria Civile, Chimica, Ambientale e dei Materiali\u2014Universit\u00e0 di Bologna, 40136 Bologna, Italy"}]},{"ORCID":"https:\/\/orcid.org\/0000-0001-9396-4519","authenticated-orcid":false,"given":"Paola","family":"Cianfarra","sequence":"additional","affiliation":[{"name":"Dipartimento di Scienze Geologiche, Universit\u00e0 degli Studi Roma Tre, 00146 Roma, Italy"}]},{"given":"Francesco","family":"Salvini","sequence":"additional","affiliation":[{"name":"Dipartimento di Scienze Geologiche, Universit\u00e0 degli Studi Roma Tre, 00146 Roma, Italy"}]},{"ORCID":"https:\/\/orcid.org\/0000-0002-8553-345X","authenticated-orcid":false,"given":"Francesco","family":"Mancini","sequence":"additional","affiliation":[{"name":"Dipartimento di Ingegneria Enzo Ferrari\u2014Universit\u00e0 degli Studi di Modena e Reggio Emilia, 41125 Modena, Italy"}]},{"given":"Paolo","family":"Sterzai","sequence":"additional","affiliation":[{"name":"Istituto Nazionale di Oceanografia e di Geofisica Sperimentale\u2014OGS\u2014\u201cInfrastructures\u201d Section (IRI), 34010 Sgonico (Trieste), Italy"}]},{"given":"Marco","family":"Dubbini","sequence":"additional","affiliation":[{"name":"Dipartimento di Storia Culture Civilt\u00e0\u2014Universit\u00e0 di Bologna, 40124 Bologna, Italy"}]},{"given":"Alessandro","family":"Capra","sequence":"additional","affiliation":[{"name":"Dipartimento di Ingegneria Enzo Ferrari\u2014Universit\u00e0 degli Studi di Modena e Reggio Emilia, 41125 Modena, Italy"}]}],"member":"1968","published-online":{"date-parts":[[2018,10,10]]},"reference":[{"key":"ref_1","doi-asserted-by":"crossref","first-page":"537","DOI":"10.1093\/gji\/ggu140","article-title":"The Antarctica component of postglacial rebound model ICE-6G_C (VM5a) based upon GPS positioning, exposure age dating of ice thicknesses, and relative sea level histories","volume":"198","author":"Argus","year":"2014","journal-title":"Geophys. 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