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Intermediate‐Depth Earthquakes Controlled by Incoming Plate Hydration Along Bending‐Related Faults
Author(s) -
Boneh Yuval,
Schottenfels Emily,
Kwong Kevin,
Zelst Iris,
Tong Xinyue,
Eimer Melody,
Miller Meghan S.,
Moresi Louis,
Warren Jessica M.,
Wiens Douglas A.,
Billen Magali,
Naliboff John,
Zhan Zhongwen
Publication year - 2019
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/2018gl081585
Subject(s) - induced seismicity , geology , seismology , slab , fault (geology) , nucleation , geophysics , chemistry , organic chemistry
Intermediate‐depth earthquakes (focal depths 70–300 km) are enigmatic with respect to their nucleation and rupture mechanism and the properties controlling their spatial distribution. Several recent studies have shown a link between intermediate‐depth earthquakes and the thermal‐petrological path of subducting slabs in relation to the stability field of hydrous minerals. Here we investigate whether the structural characteristics of incoming plates can be correlated with the intermediate‐depth seismicity rate. We quantify the structural characteristics of 17 incoming plates by estimating the maximum fault throw of bending‐related faults. Maximum fault throw exhibits a statistically significant correlation with the seismicity rate. We suggest that the correlation between fault throw and intermediate‐depth seismicity rate indicates the role of hydration of the incoming plate, with larger faults reflecting increased damage, greater fluid circulation, and thus more extensive slab hydration.