Campano-Lucano Earthquake, November 1980, Italy, Strong Motion Data Related to Local Site Conditions
Location
St. Louis, Missouri
Presentation Date
01 May 1981, 9:00 am - 12:00 pm
Abstract
When the 23 November 1980 earthquake struck the south of Italy a network of strong motion recorders was in operation. The earthquake triggered 21 stations. The network is composed by 168 stations spread all over the country following statistical criterion, see Taccarino and Zaffiro, 1973. The paper presents the results of the records obtained at 6 of 21 stations together with the available geological information of the sites where the stations were located.
Department(s)
Civil, Architectural and Environmental Engineering
Meeting Name
1st International Conference on Recent Advances in Geotechnical Earthquake Engineering and Soil Dynamics
Publisher
University of Missouri--Rolla
Document Version
Final Version
Rights
© 1981 University of Missouri--Rolla, All rights reserved.
Creative Commons Licensing
This work is licensed under a Creative Commons Attribution-Noncommercial-No Derivative Works 4.0 License.
Document Type
Article - Conference proceedings
File Type
text
Language
English
Recommended Citation
Fels, A.; Pugliese, A.; and Muzzi, F., "Campano-Lucano Earthquake, November 1980, Italy, Strong Motion Data Related to Local Site Conditions" (1981). International Conferences on Recent Advances in Geotechnical Earthquake Engineering and Soil Dynamics. 20.
https://scholarsmine.mst.edu/icrageesd/01icrageesd/session08/20
Included in
Campano-Lucano Earthquake, November 1980, Italy, Strong Motion Data Related to Local Site Conditions
St. Louis, Missouri
When the 23 November 1980 earthquake struck the south of Italy a network of strong motion recorders was in operation. The earthquake triggered 21 stations. The network is composed by 168 stations spread all over the country following statistical criterion, see Taccarino and Zaffiro, 1973. The paper presents the results of the records obtained at 6 of 21 stations together with the available geological information of the sites where the stations were located.