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Teleseismic observations of the 1976 Friuli, Italy earthquake sequence

Cipar, John (1980) Teleseismic observations of the 1976 Friuli, Italy earthquake sequence. Bulletin of the Seismological Society of America, 70 (4). pp. 963-983. ISSN 0037-1106. https://resolver.caltech.edu/CaltechAUTHORS:20140903-074831308

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Abstract

Teleseismic long-period body and surface waves radiated by the May 6, 1976 Friuli, Italy earthquake and its principal aftershock of September 15, 1976 (09h 21 m) are studied to determine source characteristics. Focal mechanisms along with geological evidence suggest that both events represent the underthrusting of the Friuli Plain beneath the southern Alps. The depths of both earthquakes, estimated by matching synthetic body-wave seismograms to observations, are found to lie between 6 and 10 km. It is not possible to discern any evidence of source directivity in the observed main shock body waves. Synthetic seismogram calculations which include rupture effects suggest that the fault length of the main shock could not be much larger than 16 km for a unilaterally propagating fault or about 24 km for a symmetrical rupture assuming a rupture velocity of 3.0 km/sec. Observations of 100-sec Rayleigh waves confirm the focal mechanism deduced from body waves, but suggest that the seismic moment of the main shock is 5 × 10^(25) dyne-cm compared to 2.9 × 10^(25) dyne-cm estimated from body waves. The P-wave moment of the aftershock is 1 × 10^(25) dyne-cm. The aftershock studied in this paper is one of four large events which occurred in the epicentral area of the main shock more than 4 months after the main shock. These aftershocks had a combined seismic moment over twice that of the main shock. It is suggested that these earthquakes represent deformation in a different part of the seismic zone than the main shock. Large earthquakes with series of severe aftershocks are well known in the historical record of the Friuli region. The average displacement and stress drop are estimated to be 33 cm and 12 bars for the main shock and 33 cm 24 bars for the aftershock.


Item Type:Article
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http://bssa.geoscienceworld.org/content/70/4/963.abstractPublisherArticle
Additional Information:© 1980 Seismological Society of America. Manuscript received November 15, 1979. The author wishes to thank John Ebel, Don Helmberger, Jim Pechmann, and Terry Wallace for critically reading the manuscript. Tom Heaton generously provided his program to compute finite fault synthetics. Laszlo Lenches and Joe Galvan drafted the figures. This research was supported by the Advanced Research Projects Agency of the Department of Defense and was monitored by the Air Force Office of Scientific Research under Contract F49620-77-C- 0022 and also by the Earth Sciences Section, National Science Foundation Grant EAR78-14786.
Funders:
Funding AgencyGrant Number
Advanced Research Projects Agency (ARPA)UNSPECIFIED
Air Force Office of Scientific Research (AFOSR)F49620-77-C-0022
NSFEAR78-14786
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Other Numbering System NameOther Numbering System ID
Caltech Division of Geological and Planetary Sciences3320
Issue or Number:4
Record Number:CaltechAUTHORS:20140903-074831308
Persistent URL:https://resolver.caltech.edu/CaltechAUTHORS:20140903-074831308
Usage Policy:No commercial reproduction, distribution, display or performance rights in this work are provided.
ID Code:49166
Collection:CaltechAUTHORS
Deposited By: Tony Diaz
Deposited On:03 Sep 2014 16:23
Last Modified:03 Oct 2019 07:11

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