Holocene coastal response to monsoons and relative sea-level changes in northeast peninsular Malaysia

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dc.contributor.authorDavid J. Mallinson
dc.contributor.authorStephen J. Culver
dc.contributor.authorD. Reide Corbett
dc.contributor.authorPeter R. Parham
dc.contributor.authorNoor Azhar Mohd Shazili
dc.contributor.authorRosnan Yaacob
dc.coverage.publicationMalaysia
dc.date.accessioned2024-05-14T04:50:44Z
dc.date.available2024-05-14T04:50:44Z
dc.date.issued2014
dc.description.abstractSedimentological, geomorphic, and ground penetrating radar (GPR) data are combined with optically stimulated luminescence data to define the Holocene evolution of a coastal system in peninsular Malaysia. The Setiu coastal region of northeast Malaysia comprises five geological and geomorphic units representing distinct evolutionary phases of this coastline.
dc.identifier.citationMallinson, D. J., Culver, S. J., Corbett, D. R., Parham, P. R., Shazili, N. A. M., & Yaacob, R. (2014). Holocene coastal response to monsoons and relative sea-level changes in northeast peninsular Malaysia. Journal of Asian Earth Sciences, 91, 194-205.
dc.identifier.urihttps://repoemc.ukm.my/handle/123456789/659
dc.languageen
dc.publisherElsevier
dc.publisher.alternativeJournal of Asian Earth Sciences
dc.subjectMalaysia
dc.subjectAsian monsoon
dc.subjectHolocene sea level
dc.subjectbeach ridges
dc.subjectground-penetrating radar
dc.subjectoptically stimulated luminescence
dc.titleHolocene coastal response to monsoons and relative sea-level changes in northeast peninsular Malaysia
dc.typeJournal

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