Anisotropy variations in the continental crust of Central – East Java region, Indonesia from local shear wave splitting

[Display omitted] •Crustal anisotropy in the CEJ region is derived from shear wave splitting analysis.•The fast directions are NE-SW to N-S and largely follow the principal strain axis.•Active faults lead the fast directions to be parallel with the strike of structures.•The anisotropy of 

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Veröffentlicht in:Journal of Asian earth sciences 2023-06, Vol.249, p.105632, Article 105632
Hauptverfasser: Muttaqy, Faiz, Dian Nugraha, Andri, Syuhada, Syuhada, Mori, James, Tyasbudi Puspito, Nanang, Trisnia Sasmi, Annisa, Supendi, Pepen, Rohadi, Supriyanto
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Sprache:eng
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Zusammenfassung:[Display omitted] •Crustal anisotropy in the CEJ region is derived from shear wave splitting analysis.•The fast directions are NE-SW to N-S and largely follow the principal strain axis.•Active faults lead the fast directions to be parallel with the strike of structures.•The anisotropy of 
ISSN:1367-9120
1878-5786
DOI:10.1016/j.jseaes.2023.105632