The 2021MW 6.2 Mamuju, West Sulawesi, Indonesia earthquake: partial rupture of the Makassar Strait thrust

Author:

Meilano Irwan1ORCID,Salman Rino2,Susilo Susilo3,Shiddiqi Hasbi Ash4ORCID,Supendi Pepen56ORCID,Lythgoe Karen2ORCID,Tay Cheryl7,Bradley Kyle2,Rahmadani Suchi18,Kristyawan Said5,Yun Sang-Ho279

Affiliation:

1. Faculty of Earth Sciences and Technology, Institute of Technology Bandung (ITB) , Bandung 40132, Indonesia

2. Earth Observatory of Singapore, Nanyang Technological University , Singapore 639798, Singapore

3. National Agency for Research and Innovation (BRIN) , Cibinong Bogor 16911, Indonesia

4. Department of Earth Science, University of Bergen , Bergen N-5020, Norway

5. Agency for Meteorology, Climatology, and Geophysics (BMKG) , Jakarta 10720, Indonesia

6. Department of Earth Sciences, University of Cambridge , Cambridge CB2 3EQ, UK

7. Asian School of the Environment, Nanyang Technological University , Singapore 639798, Singapore

8. Centre for Earthquake Science and Technology, Institute of Technology Bandung (ITB) , Bandung 40132, Indonesia

9. School of Electrical and Electronic Engineering, Nanyang Technological University , Singapore 639798, Singapore

Abstract

SUMMARYOn the 2021 January 15 (local date), an MW 6.2 earthquake struck the Mamuju and Majene regions of West Sulawesi, Indonesia. This event killed more than 100 inhabitants, leaving at least 30 000 people displaced from their homes, and damaged almost 8000 buildings within a radius of ∼30 km from the main shock's epicentre location (as shown on our damage proxy map). This event was generated by an active fault that continues to the Makassar Strait Thrust (MST) offshore West Sulawesi. The hazard potential of this fault remains poorly understood. In this study, we use seismic and Global Positioning System (GPS) data to investigate the source characteristics of the main shock. The results suggest that the main shock partially ruptured one segment of the MST, activated a secondary fault structure, and likely brought the updip unruptured section of the MST segment closure to failure. Our analysis of interseismic GPS velocities indicates that the Mamuju and Majene regions have a higher crustal strain rate than other nearby regions. The results (partial rupture of the MST segment, the updip unruptured section of the MST and high strain rate in the Mamuju and Majene regions) together suggest a significant seismic hazard potential in West Sulawesi, particularly in the Mamuju and Majene areas.

Funder

JAXA

LPDP

EOS

National Research Foundation

Publisher

Oxford University Press (OUP)

Subject

Geochemistry and Petrology,Geophysics

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