European Databases of Seismogenic Faults for Science and Engineering
Subduction
Glossaries
| Term | Main definition |
|---|---|
| Subduction | In plate tectonics a subduction zone is a region where one plate (the lower plate or slab) moves under another (the upper plate) and sinks into the mantle beneath it. This process results in a convergent movement of the two involved plates which is known to generate earthquake ruptures of different types. These ruptures are classified according to the part of the subduction zone where they occur. Interface ruptures are those that occur at the contact between the two plates; intraslab ruptures are those that occur within the slab; outer-rise ruptures also occur within the slab but in the region in front of the trench or the tip of the accretionary wedge; and splay ruptures which are those that propagate from the slab interface into the upper plate.
Hits - 1930
Synonyms:
Subduction zone Subduction system |
The work presented on this website has received funding from the European Union’s Horizon 2020 research and innovation programme under grant agreements N° 676564 (EPOS IP) and N° 730900 (SERA). It is also financially supported by the EPOS Research Infrastructure through the contribution of the Italian Ministry of University and Research (MUR) for the Joint Research Unit (JRU) EPOS-Italy.
Disclaimer: the content of this website reflects only the authors' views and our funders are not responsible for any use that may be made of the information it contains.
Except where otherwise noted, content on this site is licensed under Creative Commons Attribution-ShareAlike 4.0 International License.
Note also that each dataset distributed through this platform has its own license.
Software used
