323,268 research outputs found
Correction to: Free Diced Dorsal Augmentation (FDDA) rhinoplasty in non-caucasian patients: tips and tricks (European Journal of Plastic Surgery, (2025), 48, 1, (7), 10.1007/s00238-024-02259-1)
No full textIn this article the author’s name ‘Gianluca Marcaccini’ was incorrectly written as ‘Gianlcua Marcaccini’. Authors ‘Mirco Pozzi’ and ‘Pietro Susini’ should have been denoted as equally contributing author[s]. The original article has been corrected
Susini, Mark, Released
No full textThis record was harvested from a previous catalogue system and will be withdrawn in 2025. Information in this record may be superseded or incomplete. Visit this record in UMA's new catalogue at: https://archives.library.unimelb.edu.au/nodes/view/420027Surname: SUSINI. Given Name(s) or Initials: MARK. Military Service Number or Last Known Location: RELEASED. Missing, Wounded and Prisoner of War Enquiry Card Index Number: 180.244607
Item: [2016.0049.52288] "Susini, Mark, Released
Giancarlo Susini, Il lapidario greco e romano di Bologna
No full textD. S. G. M. Giancarlo Susini, Il lapidario greco e romano di Bologna. In: Bulletin de l'Association Guillaume Budé, n°3, octobre 1960. pp. 436-437
3D model of a sector of the South Scotia Ridge (Antarctica).
No full textthree-dimensional geological model was built to show and analyse a northern sector of the Scotia-Antarctica transform plate boundary.
The South Scotia Ridge is a 400 kill long submerged continental structural high representing the eastern continuation of the Antarctic Peninsula. South Scotia Ridge runs approximately in the E-W direction, separating Scotia Sea Plate from Antarctica Plates. Structures, due to the transform plate margin, are considered to be concentrated inside this continental high. The three-dimensional model, built using seismic profiles and a digital elevation model, is a powerful tool to visualize and help to understand deep geological structures. Maps and profiles, on the contrary, only give a two-dimensional view, and do not show the structure of the continental-oceanic boundary at depth.
The model shows that the deformation style of the continental-oceanic boundary, and of the oceanic crust nearby, is related to the left-lateral movement of the main transform fault system. Furthermore, it seems to be connected to the orientation and geometry of the South Scotia Ridge with respect to the homogeneous deformation regime, which affects the entire Scotia Plate. Moving from west to cast, the NW-dipping main fault surface becomes almost vertical with a sinistral strike-slip movement in the central sector. To the east, a south-dipping plane decreases its inclination and changes orientation (from E-W to ESE-WNW): here shortening features are visible.
The three-dimensional geological model presents a western and central province wherein the continental-oceanic boundary involves the fragmented continental blocks, the continental slope, the oceanic basement and sediments. The sedimentary cover and the oceanic basement are not deformed in the eastern province
Digital Geology from field to 3D modelling and Google Earth virtual environment: methods and goals from the Furlo Gorge (Northern Apennines – Italy)
No full textRicordo di Giancarlo Susini
No full textSi propone un ricordo dello scomparso Giancarlo Susini, studioso illustre e rigoroso cui si devono straordinarie scoperte archeologiche, come quelle sul Trasimeno, o importanti studi sulla colonizzazione romana tra il Piceno e la valle del Po, sulla guerra annibalica, sui grandi processi di acculturazione nell'età antica, sulla documentazione epigrafica, che hanno prodotto i rigorosicorporadelle iscrizioni della Cispadana, del Salento, del Dodecanneso, di altri importanti musei lapidari
Intelligent Monitoring System for Long-Term Control of Sequencing Batch Reactors
No full textThis paper discusses the application of artificial intelligence (AI) concepts to the monitoring of a lab-scale Sequencing Batch Reactor (SBR) treating nitrogen-rich wastewater (sanitary landfill leachate). The paper describes the implementation of a fuzzy inferential system to identify the correct switching sequence of the process and discusses the results obtained with six months of uninterrupted operation, during which the process conditions varied widely. The monitoring system proved capable of adjusting the process operation, in terms of phase length and external COD addition, to the varying environmental and loading conditions, with a percentage of correct phase recognition in excess of 95%. In addition, the monitoring system could be remotely operated through the internet via TCP/IP protocol
Sheet 280 – Fossombrone 3D: a study project for the new geological map of Italy at the scale of 1:50,000 in three dimensions.
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