Release of mineral-bound water prior to subduction tied to shallow seismogenic slip off Sumatra - INSU - Institut national des sciences de l'Univers Access content directly
Journal Articles Science Year : 2017

Release of mineral-bound water prior to subduction tied to shallow seismogenic slip off Sumatra

Andre Hupers
  • Function : Correspondent author
Marta E. Torres
  • Function : Author
Satoko Owari
  • Function : Author
Brandon Dugan
  • Function : Author
Kitty Milliken
  • Function : Author
Katerina E. Petronotis
  • Function : Author
Jan Backman
  • Function : Author
Sylvain Bourlange
Chen Wenhuang
  • Function : Author
Tobias A. Colson
  • Function : Author
Marina C.G. Frederik
  • Function : Author
Gilles Guérin
  • Function : Author
Mari Hamahashi
  • Function : Author
Brian M. House
  • Function : Author
Tamara N. Jeppson
  • Function : Author
Sarah Kachovich
  • Function : Author
Abby Kenigsberg
  • Function : Author
Mebae Kuranaga
  • Function : Author
Steffen Kutterolf
  • Function : Author
Freya L. Mitchison
  • Function : Author
Hideki Mukoyoshi
  • Function : Author
Nisha Nair
  • Function : Author
Kevin T. Pickering
  • Function : Author
Yehua Sahn
  • Function : Author
Insun Song
  • Function : Author
Paola Vannucchi
  • Function : Author
Peter J. Vroljik
  • Function : Author
Tao Yang
  • Function : Author
Xixi Zhao
  • Function : Author

Abstract

Plate-boundary fault rupture during the 2004 Sumatra-Andaman subduction earthquake extended closer to the trench than expected, increasing earthquake and tsunami size. International Ocean Discovery Program Expedition 362 sampled incoming sediments offshore northern Sumatra, revealing recent release of fresh water within the deep sediments. Thermal modeling links this freshening to amorphous silica dehydration driven by rapid burial-induced temperature increases in the past 9 million years. Complete dehydration of silicates is expected before plate subduction, contrasting with prevailing models for subduction seismogenesis calling for fluid production during subduction. Shallow slip offshore Sumatra appears driven by diagenetic strengthening of deeply buried fault-forming sediments, contrasting with weakening proposed for the shallow Tohoku-Oki 2011 rupture, but our results are applicable to other thickly sedimented subduction zones including those with limited earthquake records.

Domains

Earth Sciences

Dates and versions

insu-01528723 , version 1 (29-05-2017)

Identifiers

Cite

Andre Hupers, Marta E. Torres, Satoko Owari, Lisa C. Mcneill, Brandon Dugan, et al.. Release of mineral-bound water prior to subduction tied to shallow seismogenic slip off Sumatra. Science, 2017, 356 (6340), pp.841-844. ⟨10.1126/science.aal3429⟩. ⟨insu-01528723⟩
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