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10.1038/srep12110 http://scihub22266oqcxt.onion/10.1038/srep12110 C4501010!4501010!26169163     free     free     free       Sci+Rep 2015 ; 5 (ä): ä Nephropedia Template TP {{tp|p=26169163|t=2015. Normal fault earthquakes or graviquakes |pdf=|usr=}}{{26169163}} gab.com Text Normal fault earthquakes or graviquakes JO: Sci Rep http://www.kidney.de/pget.php?&tw=1&pmid=26169163 #FOAvip Earthquakes are dissipation of energy throughout elastic waves. Canonically is the elastic energy accumulated during the interseismic period. However, in crustal extensional settings, gravity is the main energy source for hangingwall fault collapsing. Gravitational potential is about 100 times larger than the observed magnitude, far more than enough to explain the earthquake. Therefore, normal faults have a different mechanism of energy accumulation and dissipation (graviquakes) with respect to other tectonic settings (strike-slip and contractional), where elastic energy allows motion even against gravity. The bigger the involved volume, the larger is their magnitude. The steeper the normal fault, the larger is the vertical displacement and the larger is the seismic energy released. Normal faults activate preferentially at about 60° but they can be shallower in low friction rocks. In low static friction rocks, the fault may partly creep dissipating gravitational energy without releasing great amount of seismic energy. The maximum volume involved by graviquakes is smaller than the other tectonic settings, being the activated fault at most about three times the hypocentre depth, explaining their higher b-value and the lower magnitude of the largest recorded events. Having different phenomenology, graviquakes show peculiar precursors. Twit Text FOAVip Normal fault earthquakes or graviquakes ????Sci Rep http://www.kidney.de/pget.php?&tw=1&pmid=26169163 #FOAvip Twit Text # Free Paper on # # # # # LINK http://www.kidney.de/pget.php?&tw=1&pmid=26169163 #FOAvip English Wikipedia <ref>{{Cite pmid|26169163}}</ref> Normal fault earthquakes or graviquakes #MMPMID26169163 Doglioni C; Carminati E; Petricca P; Riguzzi F Sci Rep 2015[]; 5 (ä): ä PMID26169163show ga Earthquakes are dissipation of energy throughout elastic waves. Canonically is the elastic energy accumulated during the interseismic period. However, in crustal extensional settings, gravity is the main energy source for hangingwall fault collapsing. Gravitational potential is about 100 times larger than the observed magnitude, far more than enough to explain the earthquake. Therefore, normal faults have a different mechanism of energy accumulation and dissipation (graviquakes) with respect to other tectonic settings (strike-slip and contractional), where elastic energy allows motion even against gravity. The bigger the involved volume, the larger is their magnitude. The steeper the normal fault, the larger is the vertical displacement and the larger is the seismic energy released. Normal faults activate preferentially at about 60° but they can be shallower in low friction rocks. In low static friction rocks, the fault may partly creep dissipating gravitational energy without releasing great amount of seismic energy. The maximum volume involved by graviquakes is smaller than the other tectonic settings, being the activated fault at most about three times the hypocentre depth, explaining their higher b-value and the lower magnitude of the largest recorded events. Having different phenomenology, graviquakes show peculiar precursors. äNormal fault earthquakes or graviquakes (epmc).pdf DeepDyve Pubget Overpricing