Crustal thickness and velocity structure of Malay Peninsula inferred from joint inversion of receiver functions and surface waves dispersion
The Malay Peninsula is located within the Sunda shelf that is subdivided geologically into three distinctive tectonic belts; western, central and eastern belts. The north-south orientation of these belts was formed during the Paleo-Tethys subduction process in the Late Paleozoic. Bentong-Raub suture...
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2019
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| Online Access: | https://www.scopus.com/inward/record.uri?eid=2-s2.0-85051378459&doi=10.1016%2fj.jseaes.2018.08.011&partnerID=40&md5=4e7f223023701c1c228e0b9044fa6fcf http://eprints.utp.edu.my/22250/ |
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