Mantle-derived helium released through the Japan trench bend-faults

Plate bending-related normal faults (i.e. bend-faults) develop at the outer trench-slope of the oceanic plate incoming into the subduction zone. Numerous geophysical studies and numerical simulations suggest that bend-faults play a key role by providing pathways for seawater to flow into the oceanic...

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Veröffentlicht in:Scientific reports 2021-06, Vol.11 (1), Article 12026
Hauptverfasser: Park, Jin-Oh, Takahata, Naoto, Hondori, Ehsan Jamali, Yamaguchi, Asuka, Kagoshima, Takanori, Tsuru, Tetsuro, Fujie, Gou, Sun, Yue, Ashi, Juichiro, Yamano, Makoto, Sano, Yuji
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