Recent GPS-based long wavelength crustal deformation revealed active postseismic deformation due to the 2006 Yogyakarta earthquake

Author:

Pratama Cecep1ORCID,Heliani Leni Sophia1,Widjajanti Nurrohmat1,Gunawan Endra2,Anjasmara Ira Mutiara3,Novianti Suci Tresna4,Sari Tika Widya4,Yuni Retno Eka4,Sekarsari Adelia4

Affiliation:

1. Department of Geodetic Engineering , 59166 Universitas Gadjah Mada , Yogyakarta , Indonesia

2. Global Geophysics Research Group, Faculty of Mining and Petroleum Engineering , Bandung Institute of Technology , Bandung , Indonesia

3. Department of Geomatics Engineering , 106242 Institut Teknologi Sepuluh Nopember , Surabaya , Indonesia

4. Study Program of Geodetic Engineering , 59166 Universitas Gadjah Mada , Yogyakarta , Indonesia

Abstract

Abstract We analyze the Global Positioning System (GPS)-derived strain rate distribution to investigate active crustal structure in Central Java, Indonesia, using ten years (2010–2019) continuous and permanent observation data. Central Java is the third-most populous province in Indonesia where postseismic deformation of devastating Yogyakarta earthquake in 2006 might influence the GPS data. The postseismic extensional response might overshadow the low contractional process due to active tectonics deformation. A decomposition method of a calculated strain rate shows a long wavelength feature with the extensional region in the vicinity of the 2006 Yogyakarta earthquake may reflect the postseismic process remain active. The short wavelength pattern is sharpening potential active tectonics dominated by oblique Northwest-Southeast dip-slip motion with East-West left-lateral sense. Our result demonstrates essential implications for assessing future seismic hazard potential within a low strain rate such as the Central Java region.

Funder

Universitas Gadjah Mada

Publisher

Walter de Gruyter GmbH

Subject

Earth and Planetary Sciences (miscellaneous),Engineering (miscellaneous),Modeling and Simulation

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