DOCSLIB.ORG

ICTP Full Technical Report 2017 CONTENTS

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
ICTP Full Technical Report 2017 CONTENTS ICTP FULL TECHNICAL REPORT 2017 INTRODUCTION This document is the full technical report of ICTP for the year 2017. For the non-technical description of 2017 highlights, please see the printed “ICTP: A Year in Review” publication. 2 ICTP Full Technical Report 2017 CONTENTS Research High Energy, Cosmology and Astroparticle Physics (HECAP) ........................................................................ 7 Director's Research Group – String Phenomenology and Cosmology ...................................... 29 Condensed Matter and Statistical Physics (CMSP)............................................................................................ 31 Mathematics ........................................................................................................................................................................ 56 Earth System Physics (ESP) ......................................................................................................................................... 64 Applied Physics Multidisciplinary Laboratory (MLab) ....................................................................................................... 89 Telecommunications/ICT for Development Laboratory (T/ICT4D) ......................................... 98 Medical Physics ................................................................................................................................................. 104 Fluid Dynamics ................................................................................................................................................... 106 Anchor Optics Research (AOR) Program............................................................................................... 107 Synchrotron Radiation Related Theory ................................................................................................. 108 Quantitative Life Sciences ........................................................................................................................................... 110 Training and Education Programmes Postgraduate Diploma Programme ........................................................................................................................ 122 ICTP-IAEA Sandwich Training Educational Programme (STEP) ............................................................. 125 Master's in Physics ........................................................................................................................................................ 129 PhD Programme in Earth Science, Fluid Dynamics and Mathematics: Interactions and Methods................................................................................................................................... 130 Joint International ICTP/SISSA PhD (JIISP) Programme in Physics and Mathematics ...................................................................................................................................... 132 Master’s in the Physics of Complex Systems ..................................................................................................... 134 Joint Master’s in High Performance Computing ………………………………………………………………… 135 Joint ICTP-UNITS Master of Advanced Studies in Medical Physics ……………………………………… 136 Career Support Associates Programme ................................................................................................................................................. 139 Federated Institutes Programme ............................................................................................................................ 147 Training and Research in Italian Laboratories (TRIL) .................................................................................. 150 ICTP-Elettra Users Programme ................................................................................................................................ 153 SESAME Programme ...................................................................................................................................................... 155 ICTP Full Technical Report 2017 3 Activities in Developing Countries Office of External Activities (OEA) .......................................................................................................................... 157 ICTP-South American Institute for Fundamental Research (ICTP-SAIFR) ......................................... 163 Mesoamerican Centre for Theoretical Physics …………………………………………………………………… 164 ICTP-East African Institute for Fundamental Research (ICTP-EAIFR)………………………………….. 166 Physics Without Frontiers…………………………………………………………………………………………………. 168 Prizes and Awards ICTP Dirac Medal ............................................................................................................................................................. 170 ICTP Prize ............................................................................................................................................................................ 170 ICO/ICTP Gallieno Denardo Award ........................................................................................................................ 170 Ramanujan Prize for Young Mathematicians from Developing Countries......................................................................................................................................... 170 Scientific Support Services Marie Curie Library ........................................................................................................................................................ 171 Information and Communication Technology Section (ICTS) ................................................................... 173 The African Review of Physics ..................................................................................................................................... 173 Science Dissemination Unit ........................................................................................................................................ 174 Appendices ICTP Statistics 2017: Visits to Research and Training Activities ................................................................................................... 182 Summary of Research and Training Activities .......................................................................................... 199 Visitors and Person-Months by Country....................................................................................................... 203 Region of Origin, ICTP Visitors .......................................................................................................................... 208 4 ICTP Full Technical Report 2017 ICTP Full Technical Report 2017 ICTP Full Technical Report 2017 5 RESEARCH 6 ICTP Full Technical Report 2017 HIGH ENERGY, COSMOLOGY AND ASTROPARTICLE PHYSICS There are four broad research areas in the High Energy, Cosmology and Astroparticle Physics Section: I. Phenomenology of Particle Physics II. Cosmology III. The ICTP ATLAS Experimental group at the CERN Large Hadron Collider IV. String and Quantum field theories I. Phenomenology of Particle Physics In 2017 the group has been active in different aspects of particle phenomenology, ranging from collider physics to studies of electric dipole moments, lepton masses and mixing, neutrinos, dark matter, axions and other light particles. 1. Collider Phenomenology: Testing the Standard Model at the Collider If new physics lies at energies above those associated to the Standard Model particles, as hinted by current collider searches, finding better ways to prove the Standard Model as a low energy effective field theory is a very important direction of research. For this purpose the group explored new ways of measuring the interactions between the vector bosons, in particular in the WZ boson production at LHC. It has been shown that the analysis of the transverse momentum distribution helps to significantly improve the sensitivity to new physics interactions. Another observable which turned out to be strongly sensitive to physics beyond the Standard Model is the azimuthal angle between the decay plane of the electroweak bosons and the scattering plane. A collider simulation has been performed to estimate the possibilities of the Large Hadron Collider to measure these interactions and it has shown that the new proposed observables can differentiate various new physics scenarios otherwise indistinguishable by the standard analysis. 2. Phenomenology of Dark Matter and New light particles QCD Axion abundance from string evolution Besides solving the strong CP problem of the Standard Model, the QCD Axion could also explain another open question of modern physics, the nature of dark matter. Depending on the primordial evolution of our Universe, axion particles could be created in different ways. In particular for high-scale inflationary scenarios the underlying symmetry associated to the axion field is expected to undergo a transition from an unbroken to a broken phase. In this scenario, configurations of so-called axionic strings form and evolve in the expanding Universe until, at the QCD cross-over scale when the axions gets a mass, strings eventually decay producing axions which would contribute the current dark matter abundance. The computation of the corresponding abundance of axions is very challenging and no agreement is currently present in the literature. Our group made an extensive study of the string evolution, performing simulations
Load more

Recommended publications
  • Fondazione Internazionale Trieste Per Il Progresso E La Libertà Delle Scienze and SISSA Interdisciplinary Laboratory
    EUROPEAN CITY OF SCIENCE 2020 Freedom for Science, Science for Freedom 1 FREEDOM FOR SCIENCE, SCIENCE FOR FREEDOM Dear Dr. Tindemans I would like to express again the support of the Italian Ministry of Education, University and Research – MIUR – to the candidature of Trieste to host the Euro Science Open forum (ESOF) in 2020. The candidature is solid and the proposed PROESOF2020 program, with the specifc goal of promoting discussion and deepening European scientifc collaboration ahead of the opening of ESOF is an unprecedented initiative represents an added value to the Valeria Fedeli proposal. Minister of Instruction, University and Research The motto “Freedom for Science, Science for Freedom”, is a refection of our times. Not only does it apply to the modern age, but it also provides guidance in the face of rapidly changing societies resulting from technological advancements and innovations, and Trieste, for it’s very well known high concentration of national and international Scientifc Institutions, functioning both as institutes of higher education as well as science and technology parks for high level research, and for both geographic and historical reasons, could not be a more ftting city to be named the European City of Science. Euro Science Open Forum would surely gain extra visibility and play an unprecedented role in the integration of Europe and in the relations between Europe and the Far-East and the South Mediterranean, and we believe that, with all its outreach and scientifc opportunities, ESOF 2020 would represent a milestone in Italy’ events to promote the role of science in society in a European context.
    [Show full text]
  • A Focal Mechanism Catalogue of Earthquakes That Occurred in The
    A focal mechanism catalogue of earthquakes that occurred in the southeastern Alps and surrounding areas from 1928 – 2019 Angela Saraò, Monica Sugan, Gianni Bressan, Gianfranco Renner, Andrea Restivo1* 5 1National Institute of Oceanography and Applied Geophysics – OGS, Italy Correspondence to: Angela Saraò ([email protected]) Abstract. We present a focal mechanism catalogue of earthquakes that occurred in the southeastern Alps and surrounding areas from 1928 to 2019. The area involved in the process of convergence between the Adria microplate and Eurasia is one of 10 the most seismically active regions in the Alpine Belt. The seismicity is minor, with the Ms=6.5 Friuli earthquake being the strongest event recorded in the area, but the seismic hazard is relevant because it is a highly populated region. For this reason, numerous studies have been carried out over time to investigate the stress field and the geodynamic characteristics of the region using focal mechanisms. To provide a comprehensive set of revised information, which is challenging to build quickly because the data is dispersed over many papers, we collected and revised the focal mechanisms that were previously published in the 15 literature. Additionally, depending on the data quality and availability, we computed new focal mechanisms by first arrival polarity inversion or seismic moment tensor. Finally, we merged all the fault plane solutions to obtain a catalogue for a selection of 772 earthquakes with 1.8 ≤ M ≤ 6.5. For each earthquake, we reported all the available focal mechanisms obtained by different authors. We also suggested a preferred solution for users who need expeditious information.
    [Show full text]
  • Study of Seismic Regime in the Alps and Dinarides Junction Zone: Block Structure Modeling and Historical Observations
    2060-48 Advanced School on Non-linear Dynamics and Earthquake Prediction 28 September - 10 October, 2009 Study of Seismic Regime in the Alps and Dinarides Junction Zone: Block Structure Modeling and Historical observations I. Vorobieva International Institute of Earthquake Prediction Theory and Mathematical Geophysics Moscow Russia Study of strong seismicity in the Alps and Dinarides Junction zone: block structure modeling and historical observations I. A. Vorobieva, A. Peresan, A. A .Soloviev and G. F. Panza. Abstract The block structure model is used to study long-term characteristics of strong seismicity at the junction zone of Alps and Dinarides. The fault-and-block geometry is outlined based on the morphostructural zoning map of the study area, as well as on the spatial pattern of the recorded seismicity. The model recovers the main features of observed seismicity and kinematics in the region that is checked against the available observations. A synthetic earthquake catalog with equivalent duration 75 thousand of years was generated,. The rate of extreme synthetic events with magnitude M17 is slightly lower than 2 events per 1000 years, and maximum magnitude is 7.4. Most of the extreme synthetic events is located along the southern boundary of Alps; another large group is located east of Istria peninsula. Several synthetic earthquakes with magnitude larger than 7 were generated along the Idrija line, and at the eastern and western boundaries of Northern Dinarides. Many of these locations already experienced significant historical earthquakes, with magnitudes greater than 6. The model evidences a number of possible locations for extreme events, where large earthquakes were not observed before; in particular several extreme events are generated at the western boundary of Dinarides nearby the city of Trieste.
    [Show full text]
  • Acquiring, Archiving, Analyzing and Exchanging Seismic Data
    ANNALS OF GEOPHYSICS, 54, 1, 2011; doi: 10.4401/ag-4958 Acquiring, archiving, analyzing and exchanging seismic data in real time at the Seismological Research Center of the OGS in Italy Pier Luigi Bragato1, Paolo Di Bartolomeo1, Damiano Pesaresi1,2,*, Milton Percy Plasencia Linares1, Angela Saraò1 1 Istituto Nazionale di Oceanografia e di Geofisica Sperimentale – OGS, Udine, Italy 2 Istituto Nazionale di Geofisica e Vulcanologia – INGV, Rome, Italy Article history Received May 5, 2010; accepted January 25, 2011. Subject classification: Surveys, measurements and monitoring, Instruments and techniques, Seismic risk, Data processing, Seismological data. ABSTRACT superimposition of several distinct strain fields that are related to different Alpine phases [e.g. Bressan et al. 2003]. The last After the 1976 Friuli earthquake (Ms = 6.5) in north-eastern Italy that severe earthquake was the 1976 Friuli earthquake, Ms = 6.5, caused about 1,000 casualties and widespread destruction in the Friuli area, which caused lot of damage and resulted in hundreds of the Italian government established the Centro di Ricerche Sismologiche casualties [Carulli and Slejko 2005, and references therein]. (CRS). This is now a department of the Istituto Nazionale di Oceanografia The Centro di Ricerche Sismologiche (CRS; Seismological e di Geofisica Sperimentale (OGS), and it is specifically devoted to the Research Center) of the Istituto Nazionale di Oceanografia e di monitoring of the seismicity of north-eastern Italy. Since its inception, the Geofisica Sperimentale (OGS) was established by the Italian North-East Italy Seismic Network has grown enormously. Currently, it government after this destructive 1976 Friuli earthquake. It consists of 14 broad-band and 20 short-period seismic stations, all of which manages an integrated seismic network (Figure 2) that is are telemetered to and acquired in real time at the OGS-CRS data center in designed to monitor regional seismic activity of north-eastern Udine.
    [Show full text]
  • Dicembre 2019 - Febbraio 2020
    ANNO 3 NUMERO 12 DICEMBRE 2019 - FEBBRAIO 2020 mappe all'interno maps inside In questo numero: In this number: In dieser Ausgabe: Civico Museo Theatrical Das Städtische Teatrale Civic Museum Theatermuseum Carlo Schmidl Carlo Schmidl Carlo Schmidl Le piazze Triest's Auf den Plätzen di Trieste Squares von Triest turistiatrieste.com turistiatrieste turistiatrieste [email protected] 1 Editoriale Indice di Anna Velia Le piazze di Trieste Triest's squares | Auf den Plätzen von Triest 6 Musei | Museums | Museen 10 Eccoci arrivati all'ultimo numero del 2019 ESOF2020 - Trieste capitale europea di Turisti a Trieste nonché all'ultimo mese della scienza 2020 dell'anno. Le luci e i colori delle bancarelle Triest Science Capital in 2020 | Triest, Hauptstadt che animeranno il centro cittadino in der Wissenschaft 2020 occasione delle festività tanto attese 14 ci faranno dimenticare il freddo della stagione invernale. Cosa c'è a tavola? What's there to eat? | Was gibt es heute zum Essen? 16 Anche questo, cari Turisti, è un buon periodo per visitare Trieste. Potrete Civico Museo Teatrale "Carlo Schmidl" apprezzare i luoghi forse meno noti che Theatrical Civic Museum | Das Städtische vi proponiamo dalle nostre pagine. E, ben Theatermuseum 26 imbacuccati nei vostri giubbotti, se avrete fortuna conoscerete la nostra famosa MAPPE | Maps | Stadtpläne bora. Così ne parlava Scipio Slataper ne 29 "Il mio Carso": Trieste Film Festival «Il monte Kal è una pietraia [...] La Trieste Film Festival | Trieste Film Festival 33 bora aguzza di schegge mi frusta e mi strappa le orecchie [...] Bella Giorni di festa è la bora. E' il tuo respiro, fratello Holidays | Feiertage 34 gigante […] Scricchia e turbina la città quando tu disfreni la tua Shopping & regali rauca anima.
    [Show full text]
  • Local Earthquake Tomography in the Junction Between South-Eastern Alps and External Dinarides Using the Seismic Data of the CE3RN Network L
    GNGTS 2015 SESSIONE 1.2 LOCAL EARTHQUAKE TOMOGRAPHY IN THE JUNCTION BETWEEN SOUTH-EASTERN ALPS AND EXTERNAL DINARIDES USING THE SEISMIC DATA OF THE CE3RN NETWORK L. Colavitti1, L. Tiberi1, G. Böhm2, G. Costa1, A. Gallo1 1 University of Trieste, Department of Mathematics and Geosciences, Seismological Research and Monitoring Group, Trieste, Italy 2 National Institute of Oceanography and Experimental Geophysics, Section of Geophysics, Trieste, Italy Introduction. The main force responsible of tectonic activity in south-eastern Alps is given by the collision between Adriatic microplate and Eurasian plate. This motion has a fundamental role in geodynamic evolution due to the convergence rate between Adria and Eurasian plate estimated greater than 2 mm/yr (Platt et al., 1989). The largest historical earthquakes occurred in the region between Italy and Slovenia are reported in Burrato et al. (2008) and Galadini et al. (2005). Several large earthquakes hit the studied region in historical times, most of them were distributed in the Friuli Venezia Giulia region, as two events recorded in Tramonti in 1776 and 1794, but the most important earthquake that spread its effects in wide region was the 1511 Idrija event that represents the most destructive event that occurred so far in the region of the junction between south-eastern Alps and the External Dinarides, as reported in the catologues (Ribarič, 1982). In general, the area of Friuli Venezia Giulia region is characterized by a moderate seismicity, in fact the most important instrumental seismic event recorded in the area was the destructive 1976 Friuli earthquake with Ms6.5 (Aoudia et al., 2000), that was widely studied thanks to the large amount of collected seismometric data.
    [Show full text]
  • The 1976 Friuli (NE Italy) Earthquake
    Giornale di Geologia Applicata 1 (2005) 147 –156, doi: 10.1474/GGA.2005-01.0-15.0015 The 1976 Friuli (NE Italy) earthquake Giovanni Battista Carulli1 & Dario Slejko2 1 Dipartimento di Scienze Geologiche, Ambientali e Marine dell’Università di Trieste 2 Istituto Nazionale di Oceanografia e di Geofisica Sperimentale - OGS, Trieste ABSTRACT. On May 6, 1976 an ML 6.4 earthquake caused about 1,000 casualties in central Friuli (where the hamlets of Gemona, Venzone, and Trasaghis suffered widespread destruction). Even though more than 25 years have passed since its occurrence, the 1976 Friuli event is still being studied. The reason for this is that it could represent the maximum possible quake in the Southern Alps and it was the first event that took place in Italy for which a large amount of seismological data were collected. Moreover, good geological and geophysical information is available for this region which also has a well- known seismological history. Nevertheless, some scientific aspects of the 1976 – 1977 seismic sequence are still under debate. This paper offers a general overview of the present knowledge about the earthquake and open the door to future investigations. Key terms: Seismicity, Neotectonics, Southern Alps, Friuli, Italy Introduction gradually towards the east into the Dinaric orogenic belt. The southern parts of these mountain chains (Carnian and The Friuli region, in NE Italy, and its surrounding areas Julian pre-Alps) face the Friuli plain to the south (the were hit by several destructive earthquakes over the eastern part of the Po plain), which can be considered their centuries, especially in the strip along the foothills foreland basin.
    [Show full text]
  • EARTHQUAKE THREAT in LJUBLJANA POTRESNA OGRO@ENOST LJUBLJANE Milan Oro`En Adami~
    EARTHQUAKE THREAT IN LJUBLJANA POTRESNA OGRO@ENOST LJUBLJANE Milan Oro`en Adami~ Crude shelter in cabbage barrels at the time of the 1895 earthquake (the Krakovsko suburb in Ljubljana, Helfer 1895). Zasilna bivali{~a v zeljarskih sodih v ~asu potresa leta 1895 (Krakovsko predmestje v Ljubljani, Helfer 1895). Geografski zbornik, XXXV (1995) Abstract UDC 550.34(497.12 Ljubljana) Earthquake Threat in Ljubljana In Slovenia, the large natural geographical units of the Alps, the Dinara Mountains, the Mediterranean, and the Pannonian basin come into contact. There have been many destructive earthquakes in this region in the past. A hundred years ago (1895), a strong earthquake with a magnitude between 8 and 9 on the MCS scale severely damaged Ljubljana. Because Ljubljana is the capital of Slovenia with the largest density of population and numerous important central functions, we consider it the zone most threatened by earthquake. A map of the microseismic zones of Ljubljana has been formulated. With the help of statistical data and other sources, we elaborated a quite detailed data base that we included in the Geographical Information System. This is the first example of such a detailed study in Slovenia, on a city area that includes about 0.9% of Slovenia's territory and 13.4% of its population. The main aim of the study was an assessment of the possible consequences of a destructive earthquake. In the most endangered zone of 9 degrees MCS are 15.23% of all the buildings in which almost 10% of Ljubljana's residents live. The assessment of earthquake vulnerability showed that in an earthquake of magnitude 9, an earthquake stronger than the one in 1895, as much as 26.3% of all the dwellings would be destroyed, and 44.9% of the dwellings would be severely damaged.
    [Show full text]
  • What Science Remains of the 1976 Friuli Earthquake?
    WhatBollettino science di Geofi remains sica ofTeorica the 1976 ed Applicata Friuli earthquake? Vol. 59, Boll.n. 4, Geof.pp. 327-350; Teor. Appl., December 59, 327-350 2018 DOI 10.4430/bgta0224 What science remains of the 1976 Friuli earthquake? D. SLEJKO Istituto Nazionale di Oceanografi a e di Geofi sica Sperimentale - OGS, Trieste, Italy (Received: 5 June 2017; accepted: 19 January 2018) ABSTRACT The main results obtained in the seismological fi eld regarding the 1976 Friuli earthquake are summarized. They refer to the source identifi cation of the main shock, to its dimension, and to the time and space evolution of the seismic sequence. Key words: 1976 earthquake, Friuli, seismic source, space and time evolution, main shock location. 1. Introduction A search on the expeditious scientifi c information available for the Belice earthquake of 1968 showed that very little is known of that earthquake (see e.g. Haas and Ayre, 1969; Monaco et al., 1996), especially as regards the seismological aspect. Conversely, a few months after the 1976 Friuli earthquake (4 and 5 December) an international scientifi c conference was held in Udine, whose acts are collected in two volumes of the international journal “Bollettino di Geofi sica Teorica ed Applicata” for a total of 1,410 pages of geology, seismology, geophysics and earthquake engineering. A year later (11-13 October 1977), the National Committee for Nuclear Energy (CNEN) organized a specialized conference in Rome on the earthquake in Friuli, also in relation to the design of nuclear installations, and the proceedings were collected in three volumes with a total of 882 pages.
    [Show full text]
  • The 1976 Friuli, Italy, Earthquake
    AIRCURRENTS THE 1976 FRIULI, ITALY, EARTHQUAKE EDITOR’S NOTE: Editor’s Note: This month marks the 35th Anniversary of a magnitude 6.4 earthquake that occurred in the Friuli region of northeast Italy. AIR director of engineering analysis and research Dr. Paolo Bazzurro describes what happened that day, its aftermath, and its lasting effects. By Dr. Paolo Bazzurro 05.2011Edited by Robert Zalisk REMEMBERING THE EVENT was just south of the the town of Gemona. It was a shallow Italy’s Friuli region rolls down the lower slopes and foothills event, estimated to have ruptured less than 20 kilometers of the eastern European Alps into the flat flood plain of below the surface. This is the most destructive kind of the River Tagliamento. To the east, today, is Slovenia, to the earthquake, as the energy it releases is closest to the human north, Austria. For centuries the foothills have been home environment. Most of Gemona was destroyed. to vineyards and small towns that in the 1960s had begun to make a transition from mostly farming to small-factory So were the nearby towns of Buia, Colloredo, Forgaria, manufacturing. The historical capital of the region, Udine, Maiano, Osoppo, Trasaghis and Venzone. In the morning, lies to the south in the fertile Friuli plain (see Figure 1). looking across Forgaria, a town of 4,000 near the Yugoslav border, a caribinieri officer described the damage as On 6 May, 1976, just before 9:00 pm, the ground began catastrophic. “Whole neighborhoods have been flattened,” to shake. The shaking lasted less than 30 seconds, but was he reported.
    [Show full text]
  • Lessons Learned After 1998 and 2004 Earthquake in Posočje Region
    Lessons learned after 1998 and 2004 earthquake in Posočje region Samo Gostič, Building and Civil Engineering Institute ZRMK email: [email protected] Blaž Dolinšek, Building and Civil Engineering Institute ZRMK email: [email protected] Summary Some information about lessons learned during reconstruction of Posočje region after earthquakes in 1998 and again in 2004 are presented. Both earthquakes were moderate (M 5.6 and M 4.9) and luckily haven’t claim death victims. But the extent of damage to the buildings and infrastructure was great. More than 3.000 buildings were reported damaged after the 1998 earthquake and about 1.800 buildings in 2004. Some of the reconstructed buildings were damaged again and that raise questions in public about reconstruction efficiency. Because the Posočje region is underdeveloped but tourist attractive region of Slovenia, the government in 1998 set up a grant scheme to help residents reconstruct their houses. The height of the grant depends on damage, public interest (ie. cultural heritage) for particular building and financial possibilities of the owner. For management of the reconstruction projects the government set up a State Technical Office. The tasks of the Office are from damage assessment and performing quick cost estimates to managing reconstruction projects (from design, construction and supervision) to accountancy. After analysis of the earthquake 2004 damage (specially damaged reconstructed buildings), some shift of renewal goals were made. The necessity of the Office remained and there were no big differences in recommended reconstruction techniques. But there were changes to grant schema – the split of costs between owner, insurance companies and government and about threshold when building is better to be replaced instead of reconstructed.
    [Show full text]
  • The 1511 Eastern Alps Earthquakes
    The 1511 Eastern Alps earthquakes: a critical update and comparison of existing macroseismic datasets Romano Camassi, Carlos Hector Caracciolo, Viviana Castelli, Dario Slejko To cite this version: Romano Camassi, Carlos Hector Caracciolo, Viviana Castelli, Dario Slejko. The 1511 Eastern Alps earthquakes: a critical update and comparison of existing macroseismic datasets. Journal of Seismol- ogy, Springer Verlag, 2010, 15 (2), pp.191-213. 10.1007/s10950-010-9220-9. hal-00652638 HAL Id: hal-00652638 https://hal.archives-ouvertes.fr/hal-00652638 Submitted on 16 Dec 2011 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Manuscript Click here to download Manuscript: camassi.doc Click here to view linked References Romano Camassi, Carlos Hector Caracciolo, Viviana Castelli, Dario Slejko, 1 2 3 4 The 1511 Eastern Alps earthquakes: a critical 5 6 7 update and comparison of existing 8 9 10 macroseismic datasets 11 12 13 14 R. Camassi [corresponding author] 15 16 17 Istituto Nazionale di Geofisica e Vulcanologia, Sezione di Bologna 18 Via Donato Creti, 12, 40128 Bologna, Italy 19 phone. +39.051.4151421 fax +39.051.4151499 20 21 22 e-mail: [email protected] 23 24 25 C.H.
    [Show full text]