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10.1038/ncomms13242 http://scihub22266oqcxt.onion/10.1038/ncomms13242 C5097125!5097125!27802263     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 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 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 2016 ; 7 (ä): ä Nephropedia Template TP {{tp|p=27802263|t=2016. Seismic evidence for a cold serpentinized mantle wedge beneath Mount St Helens |pdf=|usr=}}{{27802263}} gab.com Text Seismic evidence for a cold serpentinized mantle wedge beneath Mount St Helens JO: Nat Commun http://www.kidney.de/pget.php?&tw=1&pmid=27802263 #FOAvip Mount St Helens is the most active volcano within the Cascade arc; however, its location is unusual because it lies 50?km west of the main axis of arc volcanism. Subduction zone thermal models indicate that the down-going slab is decoupled from the overriding mantle wedge beneath the forearc, resulting in a cold mantle wedge that is unlikely to generate melt. Consequently, the forearc location of Mount St Helens raises questions regarding the extent of the cold mantle wedge and the source region of melts that are responsible for volcanism. Here using, high-resolution active-source seismic data, we show that Mount St Helens sits atop a sharp lateral boundary in Moho reflectivity. Weak-to-absent PmP reflections to the west are attributed to serpentinite in the mantle-wedge, which requires a cold hydrated mantle wedge beneath Mount St Helens (<?700?°C). These results suggest that the melt source region lies east towards Mount Adams. Twit Text FOAVip Seismic evidence for a cold serpentinized mantle wedge beneath Mount St Helens ????Nat Commun http://www.kidney.de/pget.php?&tw=1&pmid=27802263 #FOAvip Twit Text # Free Paper on # # # # # LINK http://www.kidney.de/pget.php?&tw=1&pmid=27802263 #FOAvip English Wikipedia <ref>{{Cite pmid|27802263}}</ref> Seismic evidence for a cold serpentinized mantle wedge beneath Mount St Helens #MMPMID27802263 Hansen SM; Schmandt B; Levander A; Kiser E; Vidale JE; Abers GA; Creager KC Nat Commun 2016[]; 7 (ä): ä PMID27802263show ga Mount St Helens is the most active volcano within the Cascade arc; however, its location is unusual because it lies 50?km west of the main axis of arc volcanism. Subduction zone thermal models indicate that the down-going slab is decoupled from the overriding mantle wedge beneath the forearc, resulting in a cold mantle wedge that is unlikely to generate melt. Consequently, the forearc location of Mount St Helens raises questions regarding the extent of the cold mantle wedge and the source region of melts that are responsible for volcanism. Here using, high-resolution active-source seismic data, we show that Mount St Helens sits atop a sharp lateral boundary in Moho reflectivity. Weak-to-absent PmP reflections to the west are attributed to serpentinite in the mantle-wedge, which requires a cold hydrated mantle wedge beneath Mount St Helens ( äSeismic evidence for a cold serpentinized mantle wedge beneath Mount S(epmc).pdf DeepDyve Pubget Overpricing