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Jean-Robert Grasso

Researcher at University of Grenoble

Publications -  88
Citations -  4359

Jean-Robert Grasso is an academic researcher from University of Grenoble. The author has contributed to research in topics: Induced seismicity & Aftershock. The author has an hindex of 34, co-authored 88 publications receiving 3937 citations. Previous affiliations of Jean-Robert Grasso include Joseph Fourier University & Centre national de la recherche scientifique.

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Intermittent dislocation flow in viscoplastic deformation

TL;DR: It is found that dislocations generate a slowly evolving configuration landscape which coexists with rapid collective rearrangements and should provide a framework for discussing fundamental aspects of plasticity that goes beyond standard mean-field approaches that see plastic deformation as a smooth laminar flow.
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Poroelastic stressing and induced seismicity near the Lacq gas field, southwestern France

TL;DR: In this paper, the authors compared the observed subsidence and hypocentral distributions with the predicted displacement and stress fields, and found that the relationship between average reservoir pressure drop and subsidence is remarkably linear, lending support to the linear poroelastic model.
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Probabilistic approach to rock fall hazard assessment: potential of historical data analysis

TL;DR: In this article, the authors study the rock fall volume distribution for three rock fall inventories and fit the observed data by a power-law distribution, which has recently been proposed to describe landslide and rock-fall volume distributions, and is also observed for many other natural phenomena, such as volcanic eruptions or earthquakes.
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Statistical analysis of rockfall volume distributions: Implications for rockfall dynamics

TL;DR: In this paper, the volume distribution of natural rockfalls on different geological settings (i.e., calcareous cliffs in the French Alps, Grenoble area, and granite Yosemite cliffs, California Sierra) and different volume ranges were analyzed.
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Seismic precursory patterns before a cliff collapse and critical point phenomena

TL;DR: In this paper, the authors analyse the statistical pattern of seismicity before a 1.2 103 m3 cliff collapse on the Normandie ocean shore, Western France, and show that a power law acceleration of seismic rate and energy in both 40 Hz-1.5 kHz and 2 Hz-10 kHz frequency range, is defined on 3 orders of magnitude, within 2 hours from the collapse time.