Quaternary stratigraphy and prospects for placer tin deposits in the Kuantan area, Pahang T. Suntharalingam, Ghani Ambak.

By: T. SuntharalingamContributor(s): Ghani AmbakMaterial type: TextTextPublisher: 1986Description: 1v. (various pagings) maps 30 cmSubject(s): Quaternary geology -- Kuantan -- PahangSummary: The deposits are divided into four lithostratigraphic units: the Continental Simpang Formation (equivalent to the Old Alluvium of the Kinta Valley, Pleistocene age), Kempadong Formation Unit) and the continental Beruas Formation (equivalent to the Young Alluvium of the Kinta Valley).
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Reports JMG IBUPEJABAT
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Open Shelf 551.759512331 SUN (Browse shelf) Available 0000004871
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Includes bibliographical references

The deposits are divided into four lithostratigraphic units: the Continental Simpang Formation (equivalent to the Old Alluvium of the Kinta Valley, Pleistocene age), Kempadong Formation Unit) and the continental Beruas Formation (equivalent to the Young Alluvium of the Kinta Valley).

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