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10.1038/s41467-018-05150-3 http://scihub22266oqcxt.onion/10.1038/s41467-018-05150-3 C6057928!6057928!30042446     free     free     free Deprecated: Implicit conversion from float 209.6 to int loses precision in C:\Inetpub\vhosts\kidney.de\httpdocs\pget.php on line 534 Deprecated: Implicit conversion from float 209.6 to int loses precision in C:\Inetpub\vhosts\kidney.de\httpdocs\pget.php on line 534       Nat+Commun 2018 ; 9 (ä): ä Nephropedia Template TP {{tp|p=30042446|t=2018. Rapid tremor migration and pore-pressure waves in subduction zones |pdf=|usr=}}{{30042446}} gab.com Text Rapid tremor migration and pore-pressure waves in subduction zones JO: Nat Commun http://www.kidney.de/pget.php?&tw=1&pmid=30042446 #FOAvip Rapid tremor migration (RTM) in subduction zones is a manifestation of complex fault-zone processes on the plate interface. Recent observations have revealed a large diversity of RTM patterns that are always associated with aseismic, shear strain at the interface. Small unstable asperities embedded in the stable shear zone are thus believed to originate tremor radiation during migration. Tectonic tremors have been recognized to occur where overpressured fluids exist. Spatial variations of fluid pressure may lead to non-linear diffusion processes with potentially large implications in tremor generation. Here, we show that pore-pressure waves are likely to exist in the plate interface, propagating with speeds and pathways similar to RTMs observed in different subduction zones including Guerrero, Mexico, where we introduce new high-resolution tremor locations and a RTM source physical model. These waves may explain the whole hierarchy of RTM patterns by producing transient reductions of the fault strength and thus secondary slip fronts triggering tremor during slow earthquakes. Twit Text FOAVip Rapid tremor migration and pore-pressure waves in subduction zones ????Nat Commun http://www.kidney.de/pget.php?&tw=1&pmid=30042446 #FOAvip Twit Text # Free Paper on # # # # # LINK http://www.kidney.de/pget.php?&tw=1&pmid=30042446 #FOAvip English Wikipedia <ref>{{Cite pmid|30042446}}</ref> Rapid tremor migration and pore-pressure waves in subduction zones #MMPMID30042446 Cruz-Atienza VM; Villafuerte C; Bhat HS Nat Commun 2018[]; 9 (ä): ä PMID30042446show ga Rapid tremor migration (RTM) in subduction zones is a manifestation of complex fault-zone processes on the plate interface. Recent observations have revealed a large diversity of RTM patterns that are always associated with aseismic, shear strain at the interface. Small unstable asperities embedded in the stable shear zone are thus believed to originate tremor radiation during migration. Tectonic tremors have been recognized to occur where overpressured fluids exist. Spatial variations of fluid pressure may lead to non-linear diffusion processes with potentially large implications in tremor generation. Here, we show that pore-pressure waves are likely to exist in the plate interface, propagating with speeds and pathways similar to RTMs observed in different subduction zones including Guerrero, Mexico, where we introduce new high-resolution tremor locations and a RTM source physical model. These waves may explain the whole hierarchy of RTM patterns by producing transient reductions of the fault strength and thus secondary slip fronts triggering tremor during slow earthquakes. äRapid tremor migration and pore-pressure waves in subduction zones (epmc).pdf DeepDyve Pubget Overpricing