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10.2183/pjab.93.003 http://scihub22266oqcxt.onion/10.2183/pjab.93.003 C5406623!5406623!28077808     free     free     free Warning: imagejpeg(C:\Inetpub\vhosts\kidney.de\httpdocs\phplern\28077808.jpg): Failed to open stream: No such file or directory in C:\Inetpub\vhosts\kidney.de\httpdocs\pget.php on line 117       Proc+Jpn+Acad+Ser+B+Phys+Biol+Sci 2017 ; 93 (1): 28-49 Nephropedia Template TP {{tp|p=28077808|t=2017. Rupture, waves and earthquakes |pdf=|usr=}}{{28077808}} gab.com Text Rupture, waves and earthquakes JO: Proc Jpn Acad Ser B Phys Biol Sci http://www.kidney.de/pget.php?&tw=1&pmid=28077808 #FOAvip Normally, an earthquake is considered as a phenomenon of wave energy radiation by rupture (fracture) of solid Earth. However, the physics of dynamic process around seismic sources, which may play a crucial role in the occurrence of earthquakes and generation of strong waves, has not been fully understood yet. Instead, much of former investigation in seismology evaluated earthquake characteristics in terms of kinematics that does not directly treat such dynamic aspects and usually excludes the influence of high-frequency wave components over 1 Hz. There are countless valuable research outcomes obtained through this kinematics-based approach, but ?extraordinary? phenomena that are difficult to be explained by this conventional description have been found, for instance, on the occasion of the 1995 Hyogo-ken Nanbu, Japan, earthquake, and more detailed study on rupture and wave dynamics, namely, possible mechanical characteristics of (1) rupture development around seismic sources, (2) earthquake-induced structural failures and (3) wave interaction that connects rupture (1) and failures (2), would be indispensable. Twit Text FOAVip Rupture, waves and earthquakes ????Proc Jpn Acad Ser B Phys Biol Sci http://www.kidney.de/pget.php?&tw=1&pmid=28077808 #FOAvip Twit Text # Free Paper on # # # # # LINK http://www.kidney.de/pget.php?&tw=1&pmid=28077808 #FOAvip English Wikipedia <ref>{{Cite pmid|28077808}}</ref> Rupture, waves and earthquakes #MMPMID28077808 UENISHI K Proc Jpn Acad Ser B Phys Biol Sci 2017[Jan]; 93 (1): 28-49 PMID28077808show ga Normally, an earthquake is considered as a phenomenon of wave energy radiation by rupture (fracture) of solid Earth. However, the physics of dynamic process around seismic sources, which may play a crucial role in the occurrence of earthquakes and generation of strong waves, has not been fully understood yet. Instead, much of former investigation in seismology evaluated earthquake characteristics in terms of kinematics that does not directly treat such dynamic aspects and usually excludes the influence of high-frequency wave components over 1 Hz. There are countless valuable research outcomes obtained through this kinematics-based approach, but ?extraordinary? phenomena that are difficult to be explained by this conventional description have been found, for instance, on the occasion of the 1995 Hyogo-ken Nanbu, Japan, earthquake, and more detailed study on rupture and wave dynamics, namely, possible mechanical characteristics of (1) rupture development around seismic sources, (2) earthquake-induced structural failures and (3) wave interaction that connects rupture (1) and failures (2), would be indispensable. äRupture, waves and earthquakes (epmc).pdf DeepDyve Pubget Overpricing