J. B. Scrivenor; Sea-levels in Malaya. Geological Magazine ; 83 (2): 103–104. doi:
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The evidence for a plus 50-foot sea level in Malaya is conclusive. However, that for a plus 200-foot level is shown to be based on the incorrect assumption that the sponge spicules in the rhyolite ash in Perak are marine in origin.
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