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Le acque salate dell’avanfossa marchigiana: origine, chimismo e assetto strutturale delle zone di emergenza. .
No full text30 ff., 2 tabb. Pubbl. GNDCI del CNR n. 170
Le sorgenti solfuree dell’avanfossa marchigiana.
No full text8ff.1 tabb. Pubbl. GNDCI del CNR n. 2052
Video-densitometric analysis of bone remodelling in retrospective follow-up of patients with prostheses
No full textCorrection: Groundwater circulation and earthquake-related changes in hydrogeological karst environments: a case study of the Sibillini Mountains (central Italy) involving artificial tracers (Hydrogeology Journal, (2020), 28, 7, (2409-2428), 10.1007/s10040-020-02207-w) [Correction]
No full textThe article “Groundwater circulation and earthquake-related changes in hydrogeological karst environments: a case study of the Sibillini Mountains (central Italy) involving artificial tracers”, written by T. Nanni, P. M.Vivalda, S. Palpacelli,M.Marcellini and A. Tazioli, was originally published electronically on the publisher’s internet portal on 21 July 2020 without open access. With the author(s)’ decision to opt forOpen Choice the copyright of the article changed on 13 August 2020 to © The Author(s) 2020 and the article is forthwith distributed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this licence, visit http:// creativecommons.org/licenses/by/4.0. The original article has been corrected
Analisi per imaging del rimodellamento: parte II - Applicazione a casi di artroprotesi d'anca
No full textThe mineralised springs of the Marche and Abruzzi foredeep (central Italy): some remarks on the hydrochemical and tectonics features.
No full textSome analogies between the Marche and Abruzzi mineralised waters are noticed, especially when considering the water chemical facies and the structural setting of the emergence zones 1 INTRODUCTION In many areas of the Marche and Abruzzi foredeep, salt and sulphureous waters emerge from the Messinian and Plio-Pleistocenic deposits and from the deposits of the alluvial plains. The analysis demonstrates that they are in relation with the structural setting of the emergence areas; besides, they are very numerous in zones characterised by thrusts also buried by the cover. In this study, the mineralised springs of the Marche region, already studied by the same authors (Nanni & Vivalda, 1999a; 1999b), and the Abruzzi mineralised springs, are considered. By extending the analysis to the Abruzzi sector of the Adriatic foredeep, our intent is to characterise the springs of this region on the basis of the results obtained from the previous studies, and to find possible similarities in both the water chemism and the structural setting of the emergence areas
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