Strain accumulation in the Mentawai Forearc Sliver, Indonesia, inferred from continuous GNSS-derived strain rate

Leni Sophia Heliani,Cecep Pratama,Adi Wibowo,David Prambudi Sahara, Susilo,Sidik Tri Wibowo, Ayu Nur Syafii, Oktadi Prayoga, Ajat Sudrajat,Mizan Bustanul Fuady Bisri, Evi Dwi Kurniasari, Sheilla Evelinda, Nicholas Genta Setiawan Gunawan

Geodesy and Geodynamics(2024)

Cited 0|Views6
No score
Abstract
The Mentawai Forearc Sliver (MFS) is characterized by oblique deformation formed as slip partitioned between normal and parallel trench plate convergence. The surge of great earthquakes from 2004 to 2012 along the adjacent Sunda trench left a large unbroken segment known as the Mentawai Seismic Gap. Here, we adopted continuous Global Navigation Satellite System (GNSS) observation data to identify the present regional crustal deformation using geodetic strain rates. The principal strain rate, dilatation rate, and maximum shear strain rate are about 0.13 microstrain/yr, 0.2 microstrain/yr, and 0.1 microstrain/yr, respectively, with the range of its uncertainties between 0.01 and 0.04 microstrain/yr. It is found that dilatation and maximum shear strain rates reveal the spatial coverage of strike-slip duplex and backthrust tectonics along the Mentawai Forearc Sliver.
More
Translated text
Key words
Mentawai,Forearc,Dilatation,Shear,Geodetic
AI Read Science
Must-Reading Tree
Example
Generate MRT to find the research sequence of this paper
Chat Paper
Summary is being generated by the instructions you defined