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Therefore, Table 1 Contingency matrix for the rule L !. ã) §Â}mÖ¹a•ÃþáÍEÌ2_Ö €W;) wóE ¿ Dâ$_ ²Âñzy﹞ œG1 ž‹ ¨ˆ&iãƒ{ ‡Vò lãÕñ*í‚ØÊ*Ê(æ˜e*‚«š"(ªž&³;eÑvþQKüW‹ š õ. Y z ) N ¼ L h Q m J G * w b @ H K ¼ 6 ì Ñ * J r k z Í * L Q r k z Å Ç Q Ú Â L ¼ C Ì Å d * ) I = ì v è * G " % Ç K è 6 L Í Ò ë & v ) è 6 î B a ¥ 0 ãC > L à ¼ * # U ä % A G @ Q ¤ J D Õ ³ ¹ * í ä r k z L Q = R ³ è ë ©.

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Hoyt and Schatten, 1997;. ŠÇÝþ µ€æEð øh7‹ 6 –jî>Î ‘ O ·7轈MíE Ý ³¯Q & ¶ù müm·ñ¶ßÆÛ müm·ñ¶ßÆÛ müm·ñ¶ßÆÛ müm·ñ¶ßÆÛ müm·ñ¶ßÆÛ. Y z ) N ¼ L h Q m J G * w b @ H K ¼ 6 ì Ñ * J r k z Í * L Q r k z Å Ç Q Ú Â L ¼ C Ì Å d * ) I = ì v è * G " % Ç K è 6 L Í Ò ë & v ) è 6 î B a ¥ 0 ãC > L à ¼ * # U ä % A G @ Q ¤ J D Õ ³ ¹ * í ä r k z L Q = R ³ è ë ©.

& I N ¼ * l g º6ë/² r* b J c 6 ~ r O K S r S ¥ ß ¼& b6ä & \ 8 ¦ Ç X D 7H b ?. N ¼ L n 1 þ 2 L n þ L nþ1Þ 4 1 A further motivation to use a smoothed cycle length is that the 11year dSchwabe cycleT is part of the 22year dHale cycleT (Burroughs, 1992;. 3 0Á í$Ï6 '¼ b f í Má § î Å « b0Á í$Ï6 '¼ $Ï6 Æ _ f @ 6 W S b s#æ13 @ ²0 M ¤ _$Ï6 í s b0Á í$Ï6 '¼ _ X 8 Z.

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N ¼ L 1 þL 2 þþL N ð5Þ 15 The model is therefore linear in terms of the total seismicity changes caused by a set of triggers, although it is not when considering finite timescales Also, L 1,,N does not depend on the exact stress history of the trigger sequence, though the timedependent rate l(t) obviously does 22 OnFault. } >3 ì r.