BibTex Citation Data :
@article{BFIS2974, author = {Rina Dwi Indriana}, title = {Analisis Sudut Kemiringan Lempeng Subduksi di Selatan Jawa Tengah dan Jawa Timur Berdasarkan Anomali Gravitasi dan Implikasi Tektonik Vulkanik}, journal = {BERKALA FISIKA}, volume = {11}, number = {3}, year = {2012}, keywords = {}, abstract = { Gravitation anomaly research had been done to predict the subduction dip and model. The gravitation research covered East and Central Java, Indonesia. Upward continuation used for regional anomaly mapping. Two dimension modeling from each cross-sectional used grav2poly or grav2dc. From 2D model subduction dip was calculated. The research result were subduction dip various between 3,4 0 to 8,2 0 . There is a suggestion that low magnitude of dip correlated with volcano activity and high magnitude of dip correlated with some depresstion zone. Key word: subduction zone, subduction dip, gravitation modeling }, pages = {89--96} url = {https://ejournal.undip.ac.id/index.php/berkala_fisika/article/view/2974} }
Refworks Citation Data :
Gravitation anomaly research had been done to predict the subduction dip and model. The gravitation research covered East and Central Java, Indonesia. Upward continuation used for regional anomaly mapping. Two dimension modeling from each cross-sectional used grav2poly or grav2dc. From 2D model subduction dip was calculated. The research result were subduction dip various between 3,40 to 8,20. There is a suggestion that low magnitude of dip correlated with volcano activity and high magnitude of dip correlated with some depresstion zone.
Key word: subduction zone, subduction dip, gravitation modeling
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Last update: 2024-11-20 15:40:01
Implementation of ESA-MWT method satellite gravitation data to estimate the depth of moho layer and subduction zone in Indo-Australia plate of Central Java
Alamat Penerbit/Redaksi
Departemen FisikaFakultas Sains dan Matematika Universitas DiponegoroGedung Departemen Fisika Lt. I, Kampus FSM UNDIP Tembalang Semarang 50275Telp & Fax. (024) 76480822
