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000049231 0247_ $$2DOI$$a10.1130/G21713.1
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000049231 084__ $$2WoS$$aGeology
000049231 1001_ $$0P:(DE-Juel1)VDB58242$$aChardon, D.$$b0$$uFZJ
000049231 245__ $$aFirst paleoseimological constraints on the strongest earthquake in France (Provence) in the Twentieth Century
000049231 260__ $$aMelville, NY$$bAmerican Institute of Physics$$c2005
000049231 300__ $$a901 - 904
000049231 3367_ $$0PUB:(DE-HGF)16$$2PUB:(DE-HGF)$$aJournal Article
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000049231 440_0 $$013521$$aGeology$$v33$$x0091-7613
000049231 500__ $$aRecord converted from VDB: 12.11.2012
000049231 520__ $$aWe 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.
000049231 536__ $$0G:(DE-Juel1)FUEK257$$2G:(DE-HGF)$$aChemie und Dynamik der Geo-Biosphäre$$cU01$$x0
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000049231 650_7 $$2WoSType$$aJ
000049231 65320 $$2Author$$aseismic hazard
000049231 65320 $$2Author$$aactive thrusting
000049231 65320 $$2Author$$apaleoseismology
000049231 65320 $$2Author$$aFrance
000049231 7001_ $$0P:(DE-HGF)0$$aHermitte, D.$$b1
000049231 7001_ $$0P:(DE-HGF)0$$aNguyen, F.$$b2
000049231 7001_ $$0P:(DE-HGF)0$$aBellier, O.$$b3
000049231 773__ $$0PERI:(DE-600)2041152-2$$a10.1130/G21713.1$$gVol. 33, p. 901 - 904$$p901 - 904$$q33<901 - 904$$tGeology$$v33$$x0091-7613$$y2005
000049231 8567_ $$uhttp://dx.doi.org/10.1130/G21713.1
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000049231 9141_ $$y2005
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