Active fault databases: building a bridge between earthquake geologists and seismic hazard  practitioners, the case of the QAFI v.3 database

García-Mayordomo, Julián; Martín-Banda, Raquel; Insua-Arévalo, Juan M.; Álvarez-Gómez, José A.; Martínez-Díaz, José J.; Cabral, João

doi:https://doi.org/10.5194/nhess-17-1447-2017

Articles | Volume 17, issue 8

https://doi.org/10.5194/nhess-17-1447-2017

© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.

Special issue:

Linking faults to seismic hazard assessment in Europe

https://doi.org/10.5194/nhess-17-1447-2017

© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.

Articles | Volume 17, issue 8

Review article

|

30 Aug 2017

Review article |

| 30 Aug 2017

Active fault databases: building a bridge between earthquake geologists and seismic hazard practitioners, the case of the QAFI v.3 database

Julián García-Mayordomo, Raquel Martín-Banda, Juan M. Insua-Arévalo, José A. Álvarez-Gómez, José J. Martínez-Díaz, and João Cabral

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Final revised paper (published on 30 Aug 2017)
Preprint (discussion started on 18 Apr 2017)

Interactive discussion

Status: closed

AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment

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- Supplement

RC1: 'General comments, Presentation quality and technical corrections', Edward Marc Cushing, 10 May 2017
- AC1: 'Reply to revision', JULIAN GARCIA-MAYORDOMO, 29 May 2017
RC2: 'Review comments', Nicola Litchfield, 16 May 2017
- SC1: 'Reply to revision', JULIAN GARCIA-MAYORDOMO, 29 May 2017

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision

ED: Publish subject to minor revisions (further review by Editor) (23 Jun 2017) by Bruno Pace

AR by Julian Garcia-Mayordomo on behalf of the Authors (07 Jul 2017) Author's response Manuscript

ED: Publish as is (14 Jul 2017) by Bruno Pace

Short summary

Earthquakes are produced by sudden movements of rock masses along surfaces called faults. Major earthquakes are produced by major faults. It is important to know where these faults are located in a territory. Major faults can be seen in the landscape as they control the morphology of the terrain. In the field geologists determine their last movement and the rate they move at over time. This information is stored in active fault databases and later used for earthquake prevention.