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Evidence for Quaternary environmental changes from sea-floor sediments in Hong Kong in Palaeoenvironmental Conference of East Asia from the mid-Tertiary.
(supprimer)
Evidence for Quaternary environmental changes from sea-floor sediments in HongKong in Palaeoenvironmental Conference of East Asia from the mid-Tertiary.
on the Quaternary environmental changes in Hong-Kong. A similar sedimentary sequence is recognized at three separate localities. The type sequence is from top to bottom 1) upper marine deposits of Holocene age post-dating about 8 000 years BP| 2) upper alluvial