细丝
发表于 2025-3-25 05:26:23
Hansjörg Rohdetion of some objects on the ground surface – were explained as being caused by the consecutive inc- nations and recovery of these objects to the vertical, when hit by the in- dent seismic body or surface wav978-3-642-06843-0978-3-540-31337-3
激怒
发表于 2025-3-25 11:14:56
make them vibrate out-of-phase under seismic excitation. In contrast, in the case of longer bridge structures, it is more often the seismic wave propagation effect that induces collisions between superstructure segments during earthquakes..978-3-319-35829-1978-3-319-16324-6Series ISSN 2190-5193 Series E-ISSN 2190-5207
变白
发表于 2025-3-25 14:18:31
1616-0770 mmenfassung der Ergebnisse für unmodulierte Laserpulse 6) Experimentelle Ergebnisse zum Einzelpulsbohren mit adaptierten Laserpulsen - Berechnete Austrittsdurch978-3-519-06243-1978-3-322-96733-6Series ISSN 1616-0770
FLAT
发表于 2025-3-25 17:31:38
http://reply.papertrans.cn/79/7805/780490/780490_24.png
Nausea
发表于 2025-3-25 21:45:21
Book 1999enhänge - Einfluß der Fokusgeometrie - Einfluß der Pulsdauer - Einfluß des Gasdrucks - Einfluß der Fokuslage - Einfluß der Intensität - Zusammenfassung der Ergebnisse für unmodulierte Laserpulse 6) Experimentelle Ergebnisse zum Einzelpulsbohren mit adaptierten Laserpulsen - Berechnete Austrittsdurch
dithiolethione
发表于 2025-3-26 00:19:15
Qualitätsbestimmende Prozeßparameter beim Einzelpulsbohren mit einem Nd:YAG-Slablaser
sundowning
发表于 2025-3-26 06:35:59
Hansjörg Rohde of different inertia moments of an inflicted body. Thus, the surface rotation effects – rotation of some objects on the ground surface – were explained as being caused by the consecutive inc- nations and recovery of these objects to the vertical, when hit by the in- dent seismic body or surface wav
conference
发表于 2025-3-26 10:07:36
http://reply.papertrans.cn/79/7805/780490/780490_28.png
Feature
发表于 2025-3-26 16:39:16
http://reply.papertrans.cn/79/7805/780490/780490_29.png
synchronous
发表于 2025-3-26 20:23:14
Hansjörg Rohde km away. Flow of unconsolidated volcanic sediment and rock failures of consolidated bedrock occurred at locations 200–300 km away. These indicate that magnitude 8 is the line of demarcation at which the relationship between the distance from the epicenter to landslide sites and the movement types c