z-logo
open-access-imgOpen Access
Earthquakes track subduction fluids from slab source to mantle wedge sink
Author(s) -
Felix Halpaap,
S. Rondenay,
Alexander Perrin,
Saskia Goes,
Lars Ottemöller,
Håkon Austrheim,
Robert K. Shaw,
Thomas Eeken
Publication year - 2019
Publication title -
science advances
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 5.928
H-Index - 146
ISSN - 2375-2548
DOI - 10.1126/sciadv.aav7369
Subject(s) - geology , slab , subduction , mantle wedge , mantle (geology) , seismology , induced seismicity , sink (geography) , wedge (geometry) , geophysics , petrology , tectonics , physics , cartography , optics , geography
Fluids trigger earthquakes as they flow upward along the subducted slab and escape into the overlying rocks.

The content you want is available to Zendy users.

Already have an account? Click here to sign in.
Having issues? You can contact us here
Accelerating Research

Address

John Eccles House
Robert Robinson Avenue,
Oxford Science Park, Oxford
OX4 4GP, United Kingdom