Crustal velocity structure in Borneo Island using receiver function inversion
Author:
Publisher
Springer Science and Business Media LLC
Subject
Geophysics
Link
https://link.springer.com/content/pdf/10.1007/s11600-022-00870-z.pdf
Reference90 articles.
1. Ahmed N, Siddiqui NA, Sanaullah M, Jamil M et al (2021) The Bawang member, a unique unit of Belaga Formation in the Miri Zone, Central Sarawak, NW Borneo Malaysia: revised stratigraphic and sedimentological characteristics. J Nat Gas Geosci 6:27–42. https://doi.org/10.1016/j.jnggs.2021.02.001
2. Ammon CJ (1991) The isolation of receiver eAects from teleseismic P waveforms. Bull Seismol Soc Am 81:2504–2510. https://doi.org/10.1785/bssa0810062504
3. Anggono T, Syuhada S, Febriani F et al (2020) Crustal shear-wave velocity structure in Western Java, Indonesia from analysis of teleseismic receiver functions. J Earth Syst Sci. https://doi.org/10.1007/s12040-019-1288-1
4. Advokaat EL, Marshall NT, Li S et al (2018) Cenozoic rotation history of Borneo and Sundaland, SE Asia revealed by paleomagnetism, seismic tomography, and kinematic reconstruction. Tectonics 37:2486–2512. https://doi.org/10.1029/2018tc005010
5. Balaguru A, Nichols G (2004) Tertiary stratigraphy and basin evolution, southern Sabah (Malaysian Borneo). J Asian Earth Sci 23:537–554. https://doi.org/10.1016/j.jseaes.2003.08.001
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