Energy release and seismic flux
TL;DRAbstract
From the basic data and tlie previous results of priorpapers, we have made evaluations of the energy released and studied itsvariation. Its pulsative form is confirmed, which suggests several superposedperiods, perhaps of simple multiples of tlie undecenal of solar activity.For steps of a whole unity of m, the total approximated energy is computed.EN and Et may be compared, it being possible to replace one by the other,indifferently, from m = 5 up to m = 7.5. The compared variation of logEN with N demostrates they are not proportional.The tectonic flux is evaluated and we have the graphs for 5 and 15year lapses, from 1901 to I960, as well as another graph which correspondsto the representative average of these 60 years. A reduction of the mapof seismic activity attained through log (2 E)li2-. 60 x 2.5 is attached, whichrefers the annual flux for every 1000 sq km. This map is analyzed and thecomparative results with the zones of the first seismotectonic sketch publishedby Rey Pastor (19
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From the basic data and tlie previous results of priorpapers, we have made evaluations of the energy released and studied itsvariation. Its pulsative form is confirmed, which suggests several superposedperiods, perhaps of simple multiples of tlie undecenal of solar activity.For steps of a whole unity of m, the total approximated energy is computed.EN and Et may be compared, it being possible to replace one by the other,indifferently, from m = 5 up to m = 7.5. The compared variation of logEN with N demostrates they are not proportional.The tectonic flux is evaluated and we have the graphs for 5 and 15year lapses, from 1901 to I960, as well as another graph which correspondsto the representative average of these 60 years. A reduction of the mapof seismic activity attained through log (2 E)li2-. 60 x 2.5 is attached, whichrefers the annual flux for every 1000 sq km. This map is analyzed and thecomparative results with the zones of the first seismotectonic sketch publishedby Rey Pastor (19
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