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Emmel, Frans J., Curray, Joseph R. (1982) A submerged late Pleistocene delta and other features related to sea level changes in the Malacca Strait. Marine Geology, 47 (3) 197-216 doi:10.1016/0025-3227(82)90069-x

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Reference TypeJournal (article/letter/editorial)
TitleA submerged late Pleistocene delta and other features related to sea level changes in the Malacca Strait
JournalMarine Geology
AuthorsEmmel, Frans J.Author
Curray, Joseph R.Author
Year1982 (June)Volume47
Issue3
PublisherElsevier BV
DOIdoi:10.1016/0025-3227(82)90069-xSearch in ResearchGate
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Mindat Ref. ID548639Long-form Identifiermindat:1:5:548639:1
GUID0
Full ReferenceEmmel, Frans J., Curray, Joseph R. (1982) A submerged late Pleistocene delta and other features related to sea level changes in the Malacca Strait. Marine Geology, 47 (3) 197-216 doi:10.1016/0025-3227(82)90069-x
Plain TextEmmel, Frans J., Curray, Joseph R. (1982) A submerged late Pleistocene delta and other features related to sea level changes in the Malacca Strait. Marine Geology, 47 (3) 197-216 doi:10.1016/0025-3227(82)90069-x
In(1982, June) Marine Geology Vol. 47 (3) Elsevier BV

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Curray, Joseph R., Emmel, Frans J. (1981) Demise of the Diamantina Dent. Marine Geology, 40 (3) doi:10.1016/0025-3227(81)90140-7
Kudrass, H.R, Schlüter, H.U (1994) Development of cassiterite-bearing sediments and their relation to late Pleistocene sea-level changes in the Straits of Malacca. Marine Geology, 120 (3) 175-202 doi:10.1016/0025-3227(94)90058-2
Moore, David G., Curray, Joseph R., Emmel, Frans J. (1976) Large submarine slide (olistostrome) associated with Sunda Arc subduction zone, northeast Indian Ocean. Marine Geology, 21 (3) 211-226 doi:10.1016/0025-3227(76)90060-8
Szabo, Barney J (1982) Age determination of late Pleistocene marine transgression in western Alaska. Marine Geology, 46 (1) doi:10.1016/0025-3227(82)90147-5
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GEYH, M. A., STREIF, H., KUDRASS, H.-R. (1979) Sea-level changes during the late Pleistocene and Holocene in the Strait of Malacca. Nature, 278 (5703). 441-443 doi:10.1038/278441a0
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