Development and Operation of a Regional Moment Tensor Analysis System in the Philippines: Contributions to the Understanding of Recent Damaging Earthquakes

• Published in: Journal of disaster research 2015-02, Vol.10 (1), p.25-34
• Main Authors: Punongbayan, Baby Jane T., Kumagai, Hiroyuki, Pulido, Nelson, Bonita, Jun D., Nakano, Masaru, Yamashina, Tadashi, Maeda, Yuta, Inoue, Hiroshi, Melosantos, Arnaldo A., Figueroa, Melquiades F., Alcones, Ponczh Colleen M., Soriano, Karl Vincent C., Narag, Ishmael C., Solidum, Renato U., Jr
• Format: Article
• Language: English
• ISSN: 1881-2473; 1883-8030
• DOI: 10.20965/jdr.2015.p0025

A network of 10 satellite-telemetered broadband stations was established under a cooperative project between Japan and the Philippines, and a source analysis system based on waveform inversion of regional seismograms was adapted to operationalize a regional moment tensor analysis of Philippine earthquakes. This study presents the source information generated by the system for recent damaging earthquakes: the M w 6.7 Negros and M w 7.6 offshore Samar in 2012, and the M w 7.2 in Bohol in 2013. Results show that the Negros event was generated by shallow NE–SW thrust faulting with a small strike-slip component, and that the centroid was located slightly offshore. The Samar event occurred in relation to an outer-trench thrust fault within the Philippine Sea Plate, adjacent to a part of the Philippine Trench that has relatively low seismicity. Our centroid moment tensor (CMT) solutions show that the Samar event triggered distinct clusters of outer-rise normal and thrust aftershocks, which we explain as being consistent with a Coulomb stress change in the area. Finally, we infer that the previously unidentified fault zone that generated the Bohol earthquake has a length of ∼ 100 km, is oriented ENE–WSW, transects parts of Bohol, and extends offshore towards Cebu. These examples show how recent improvements in Philippine earthquake monitoring could contribute to the characterization of earthquake sources and in the understanding of the seismotectonics of the area.