Release of mineral-bound water prior to subduction tied to shallow seismogenic slip off Sumatra
Multidisciplinary
Science & Technology
STRESS
550
PRISM
[SDU.STU]Sciences of the Universe [physics]/Earth Sciences
ZONE
01 natural sciences
Multidisciplinary Sciences
MODEL
MEGATHRUST
RUPTURE
13. Climate action
1000 General
[SDU.STU] Sciences of the Universe [physics]/Earth Sciences
Science & Technology - Other Topics
ANDAMAN EARTHQUAKE
Multidisciplinary, seismogenesis, tsunami, Sumatra
14. Life underwater
PORE PRESSURE
SEDIMENTS
0105 earth and related environmental sciences
DOI:
10.1126/science.aal3429
Publication Date:
2017-05-25T21:40:11Z
AUTHORS (33)
ABSTRACT
Plate-boundary fault rupture during the 2004 Sumatra-Andaman subduction earthquake extended closer to trench than expected, increasing and tsunami size. International Ocean Discovery Program Expedition 362 sampled incoming sediments offshore northern Sumatra, revealing recent release of fresh water within deep sediments. Thermal modeling links this freshening amorphous silica dehydration driven by rapid burial-induced temperature increases in past 9 million years. Complete silicates is expected before plate subduction, contrasting with prevailing models for seismogenesis calling fluid production subduction. Shallow slip Sumatra appears diagenetic strengthening deeply buried fault-forming sediments, weakening proposed shallow Tohoku-Oki 2011 rupture, but our results are applicable other thickly sedimented zones including those limited records.
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