失望未来
发表于 2025-3-25 03:29:56
http://reply.papertrans.cn/87/8639/863854/863854_21.png
entreat
发表于 2025-3-25 09:26:57
Book 1985c processes causing the Liege events. 2. Seismic Station Network During the period of 1976 to 1982 the seismic station network in the Lower Rhine Embayment and in the Rhenish Massif was consi= derably enlarged and mostly equipped with digital recording systems (Figure 1). At present there are more t
hegemony
发表于 2025-3-25 11:42:15
http://reply.papertrans.cn/87/8639/863854/863854_23.png
商业上
发表于 2025-3-25 17:44:35
http://reply.papertrans.cn/87/8639/863854/863854_24.png
LIEN
发表于 2025-3-25 20:57:03
http://reply.papertrans.cn/87/8639/863854/863854_25.png
TSH582
发表于 2025-3-26 02:56:43
http://reply.papertrans.cn/87/8639/863854/863854_26.png
吸引人的花招
发表于 2025-3-26 04:30:05
http://reply.papertrans.cn/87/8639/863854/863854_27.png
痛恨
发表于 2025-3-26 08:44:58
Intraplate Seismic Activity in the Brabant Massif and the Graben Systems of Lower Rhine-Roer and Norte for magnitude 6 earthquakes in the total region is of the order of 60–100 years. Locally this time of recurrence is 10–100 times longer. Co-operative measures in seismic data acquisition and exchange, and in scientific investigations in the field are advocated
Bravura
发表于 2025-3-26 15:04:20
The Earthquakes of Liege of November 8, 1983 and December 21, 1965f the local magnitude determined by the coda duration measurement at the belgian seismological stations is M. = 5.0 which is comparable to the values given by other networks..Supposing the source being a circular crack, the radius has been estimated to 1200 m, the stress drop to 40 bars and the seismic moment 1.5 10. dyne.cm.
泥沼
发表于 2025-3-26 18:13:21
http://reply.papertrans.cn/87/8639/863854/863854_30.png