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Geodetic strain to study the deformation model of Indonesian semi dynamic datum 2013
Susiloa,b, Meilano I.a, Abidin H.Z.a,b, Sarsito D.A.b, Sapiie B.b, Efendi J.a
a Geospatial Information Agency, Cibinong, 16911, Indonesia
b Bandung Institute of Technology, Bandung, Indonesia
[vc_row][vc_column][vc_row_inner][vc_column_inner][vc_separator css=”.vc_custom_1624529070653{padding-top: 30px !important;padding-bottom: 30px !important;}”][/vc_column_inner][/vc_row_inner][vc_row_inner layout=”boxed”][vc_column_inner width=”3/4″ css=”.vc_custom_1624695412187{border-right-width: 1px !important;border-right-color: #dddddd !important;border-right-style: solid !important;border-radius: 1px !important;}”][vc_empty_space][megatron_heading title=”Abstract” size=”size-sm” text_align=”text-left”][vc_column_text]© 2018 Author(s).Indonesia is located in the very complex and active tectonic region and therefore prone to various natural hazards which caused a surface deformation. Accordingly, on the development of geodetic datum of Indonesia should take into account this conditions. Indonesian Geospatial Reference System 2013 (IGRS2013) is a semi dynamic geodetic datum that accounted the surface deformation in the form of deformation model. In order to build a deformation model of IGRS2013, its very important to study a strain rate model. In this study, we use a GPS velocities data to determine strain rate model in the Indonesia region. Our analysis reveals that Indonesia region characterized by mostly shortening strain patterns in the western Indonesia, very complex strain patterns in the eastern Indonesia with shortening and extension, while the Sunda land strain patterns show the stable area. This information is useful to supporting the development of IGRS2013 deformation model and disaster mitigation.[/vc_column_text][vc_empty_space][vc_separator css=”.vc_custom_1624528584150{padding-top: 25px !important;padding-bottom: 25px !important;}”][vc_empty_space][megatron_heading title=”Author keywords” size=”size-sm” text_align=”text-left”][vc_column_text][/vc_column_text][vc_empty_space][vc_separator css=”.vc_custom_1624528584150{padding-top: 25px !important;padding-bottom: 25px !important;}”][vc_empty_space][megatron_heading title=”Indexed keywords” size=”size-sm” text_align=”text-left”][vc_column_text]geodetic strain,IGRS2013,Indonesia,semi dynamic datum[/vc_column_text][vc_empty_space][vc_separator css=”.vc_custom_1624528584150{padding-top: 25px !important;padding-bottom: 25px !important;}”][vc_empty_space][megatron_heading title=”Funding details” size=”size-sm” text_align=”text-left”][vc_column_text]We thank an anonymous reviewer and the Editor for their thoughtful and thorough reviews. This research is partially supported by Research and Innovation No. FITB.PN-6-03-2017 ITB, Global Research on Earthquake, Active Tectonic ITB, Badan Informasi Geospasial. Figures in this manuscript were generated using the Generic Mapping Tool [9].[/vc_column_text][vc_empty_space][vc_separator css=”.vc_custom_1624528584150{padding-top: 25px !important;padding-bottom: 25px !important;}”][vc_empty_space][megatron_heading title=”DOI” size=”size-sm” text_align=”text-left”][vc_column_text]https://doi.org/10.1063/1.5047387[/vc_column_text][/vc_column_inner][vc_column_inner width=”1/4″][vc_column_text]Widget Plumx[/vc_column_text][/vc_column_inner][/vc_row_inner][/vc_column][/vc_row][vc_row][vc_column][vc_separator css=”.vc_custom_1624528584150{padding-top: 25px !important;padding-bottom: 25px !important;}”][/vc_column][/vc_row]