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@ARTICLE{Chardon:49231,
author = {Chardon, D. and Hermitte, D. and Nguyen, F. and Bellier,
O.},
title = {{F}irst paleoseimological constraints on the strongest
earthquake in {F}rance ({P}rovence) in the {T}wentieth
{C}entury},
journal = {Geology},
volume = {33},
issn = {0091-7613},
address = {Melville, NY},
publisher = {American Institute of Physics},
reportid = {PreJuSER-49231},
pages = {901 - 904},
year = {2005},
note = {Record converted from VDB: 12.11.2012},
abstract = {We have identified surface ruptures of M >= 6 earthquakes
on a branch of the propagating reverse fault system that
produced the strongest event recorded in France during the
twentieth century (1909 Lambesc earthquake, Provence). The
rate of slip on that branch is 0.05-0.3 mm/yr with a
corresponding return period for M >= 6 events of 700-5000
yr. In addition to possibly identifying the 1909 earthquake
surface rupture, by recognizing successive surface breaks of
large earthquakes, this study calls for a reassessment of
seismic hazard in Provence.},
keywords = {J (WoSType)},
cin = {ICG-IV},
ddc = {550},
cid = {I:(DE-Juel1)VDB50},
pnm = {Chemie und Dynamik der Geo-Biosphäre},
pid = {G:(DE-Juel1)FUEK257},
shelfmark = {Geology},
typ = {PUB:(DE-HGF)16},
UT = {WOS:000233059000016},
doi = {10.1130/G21713.1},
url = {https://juser.fz-juelich.de/record/49231},
}