@article{fdi:010084228, title = {{S}eismotectonics of southeast {F}rance : from the {J}ura mountains to {C}orsica}, author = {{L}arroque, {C}. and {B}aize, {S}. and {A}lbaric, {J}. and {J}omard, {H}. and {T}revisan, {J}. and {G}odano, {M}. and {C}ushing, {M}. and {D}eschamps, {A}. and {S}ue, {C}. and {D}elouis, {B}. and {P}otin, {B}. and {C}ourboulex, {F}. and {R}{\'e}gnier, {M}arc and {R}ivet, {D}. and {B}runel, {D}. and {C}heze, {J}. and {M}artin, {X}. and {M}aron, {C}. and {P}eix, {F}.}, editor = {}, language = {{ENG}}, abstract = {{T}he analysis of the seismicity catalog (1996 to 2019) covering the region from the {J}ura mountains to {C}orsica provides a first-order image of the distribution of earthquakes, highlighting large structures such as the {B}rianconnais and {P}iedmontais seismic arcs, the eastward deepening of the focal depths through the {W}estern {A}lps, several large active faults (e.g. {B}elledonne. {M}iddle {D}urance, {L}igure). {O}ver this period the magnitudes are moderate and the focal mechanisms of the main events display a diversity of seismic behaviors that can be explained by the complexity of the different geological domains with a more or less strong structural inheritage, by variable theological characteristics at the scale of the crust and by the joint action of different mechanisms of deformation. {T}he distribution of the historical events is in fairly good agreement with the instrumental seismicity, but several earthquakes of {M} > 6 are highlighted since the 14th century until the beginning of the 20th.}, keywords = {{E}arthquakes ; {F}aults ; {J}ura-{B}resse ; {S}outheast basin ; {W}estern {A}lps ; {L}igurian {S}ea ; {C}orsica ; {FRANCE} ; {MEDITERRANEE} ; {CORSE} ; {JURA} ; {BRESSE} ; {ALPES} ; {LIGURIE} {MER}}, booktitle = {{S}eismicity in {F}rance}, journal = {{C}omptes {R}endus {G}eoscience}, volume = {353}, numero = {{S}1}, pages = {105--151}, ISSN = {1631-0713}, year = {2021}, DOI = {10.5802/crgeos.69}, URL = {https://www.documentation.ird.fr/hor/fdi:010084228}, }