NGA-Sub source and path database

Author:

Contreras Victor12,Stewart Jonathan P1ORCID,Kishida Tadahiro3ORCID,Darragh Robert B4,Chiou Brian SJ5,Mazzoni Silvia1,Youngs Robert R6,Kuehn Nicolas M1,Ahdi Sean K1ORCID,Wooddell Katie7,Boroschek Rubén8,Rojas Fabián8,Órdenes Jennyfer8

Affiliation:

1. University of California, Los Angeles, Los Angeles, CA, USA

2. Universidad Diego Portales, Santiago, Chile

3. Khalifa University of Science Technology and Research, Abu Dhabi, UAE

4. Pacific Engineering and Analysis, El Cerrito, CA, USA

5. California Department of Transportation, Sacramento, CA, USA

6. Wood PLC, Oakland, CA, USA

7. Slate Geotechnical Consultants, Berkeley, CA, USA

8. University of Chile, Santiago, Chile

Abstract

We describe source and path attributes of the Next Generation of Ground-Motion Attenuation for Subduction zones (NGA-Sub) project relational database. The database contains 991 earthquakes between 1937 and 2016 that meet quality assurance standards and have assigned event types (mostly interface or intraslab). Data curation emphasized large magnitudes: 73% of events have M > 5 and 13 events have M > 8. Event attributes in the database can be broadly divided into those related to the moment tensor, those related to rupture surface geometry (referred to as finite-fault parameters), and categorizations by type (e.g. interface, intraslab) and sequence classification (mainshock, aftershock). Earthquake information and moment tensor parameters compiled from earthquake catalogs include event date and origin time, hypocenter location, seismic moment, and the strike, dip, and rake angles of nodal planes. Finite-fault parameters include along-strike length, down-dip width, and depth to top-of-rupture for one or more rectangles used to parameterize rupture surface geometry. These are modified from models in literature where available, and otherwise are simulated using procedures customized for subduction earthquakes. Rupture distance and other metrics are computed using finite-fault representations of sources, and (as applicable) are partitioned into forearc and backarc components. Forearc and backarc regions are defined based on volcano locations, and are assigned to events and sites.

Funder

the California Department of Transportation

University of California

Publisher

SAGE Publications

Subject

Geophysics,Geotechnical Engineering and Engineering Geology

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