Ontology highlight
ABSTRACT:
SUBMITTER: Audet P
PROVIDER: S-EPMC5846282 | biostudies-literature | 2018 Mar
REPOSITORIES: biostudies-literature
Science advances 20180307 3
At subduction zones, the deep seismogenic transition from a frictionally locked to steady sliding interface is thought to primarily reflect changes in rheology and fluid pressure and is generally located offshore. The development of fluid pressures within a seismic low-velocity layer (LVL) remains poorly constrained due to the scarcity of dense, continuous onshore-offshore broadband seismic arrays. We image the subducting Juan de Fuca oceanic plate in northern Cascadia using onshore-offshore tel ...[more]