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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Bibliographic Details
Main Authors: Abdul Latiff, A.H., Khalil, A.E.
Format: Article
Published: 2019
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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Institution: Universiti Teknologi Petronas