Significant duration of strong shaking quantifies the length of time during which strong earthquake-induced shaking occurs at a given site. Significant duration has multiple applications in Geotechnical and Structural Engineering. However, while multiple ground motion prediction (GMPE) equations for duration exist for shallow crustal tectonic environments, at the time of this publication, there are few published models for predicting significant duration of subduction earthquakes. To address this need and to identify the difference between significant duration of motions resulting from earthquakes in different tectonic regimes, we develop predictive equations for significant duration applicable to interface and intraslab subduction earthquakes and shallow crustal earthquakes in active tectonic regimes using the KiK-net ground motion database. The GMPEs are applicable to earthquakes with M4 to 9. In addition, the influence of earthquake magnitude on duration due to path effects is captured in the proposed relationships. Based on the relationships proposed in this study, we note that the duration of ground motions from subduction earthquakes is longer than those of shallow crustal earthquakes that have similar magnitudes and distances. The predictions of duration for shallow crustal earthquakes in active tectonic regimes developed in this study are consistent with those from previous studies.
Skip Nav Destination
Article navigation
Research Article|
May 01, 2021
Ground motion prediction equations for significant duration using the KiK-net database
Mahdi Bahrampouri, M.EERI;
Mahdi Bahrampouri, The Charles E. Via, Jr. Department of Civil and Environmental Engineering, Virginia Tech, 750 Drillfield Drive, Patton Hall, Blacksburg, VA 24061, USA. Email: mahdibp@vt.edu
Search for other works by this author on:
Adrian Rodriguez-Marek, M.EERI;
Adrian Rodriguez-Marek, M.EERI
Search for other works by this author on:
Earthquake Spectra (2021) 37 (2): 903–920.
Article history
received:
20 Oct 2019
accepted:
22 Aug 2020
first online:
17 Nov 2021
Citation
Mahdi Bahrampouri, Adrian Rodriguez-Marek, Russell A Green; Ground motion prediction equations for significant duration using the KiK-net database. Earthquake Spectra 2021;; 37 (2): 903–920. doi: https://doi.org/10.1177/8755293020970971
Download citation file:
You could not be signed in. Please check your email address / username and password and try again.
Email alerts
Index Terms/Descriptors
Citing articles via
Related Articles
BC Hydro Ground Motion Prediction Equations for Subduction Earthquakes
Earthquake Spectra
A Method for Including Path Effects in Ground‐Motion Prediction Equations: An Example Using the Mw 9.0 Tohoku Earthquake Aftershocks
Bulletin of the Seismological Society of America
A suite of ground motion prediction equations for cumulative absolute velocity in shallow crustal earthquakes including epistemic uncertainty
Earthquake Spectra
Ground‐Motion Prediction Equations of Intermediate‐Depth Earthquakes in the Hellenic Arc, Southern Aegean Subduction Area
Bulletin of the Seismological Society of America
Related Book Content
Chapter 3.2b Bransfield Strait and James Ross Island: petrology
Volcanism in Antarctica: 200 Million Years of Subduction, Rifting and Continental Break-up
Styles of underplating in the Marin Headlands terrane, Franciscan complex, California
Geology and Tectonics of Subduction Zones: A Tribute to Gaku Kimura
Upper-plate tectonic hysteresis and segmentation of the rupture area during seismogenesis in subduction zones—A case study of the Nankai Trough
Geology and Tectonics of Subduction Zones: A Tribute to Gaku Kimura
Tectonics: 50 years after the Revolution
The Web of Geological Sciences: Advances, Impacts, and Interactions
Anatomy and global context of the North American Cordillera
Backbone of the Americas: Shallow Subduction, Plateau Uplift, and Ridge and Terrane Collision
Shallowing and steepening subduction zones, continental lithospheric loss, magmatism, and crustal flow under the Central Andean Altiplano-Puna Plateau
Backbone of the Americas: Shallow Subduction, Plateau Uplift, and Ridge and Terrane Collision