Pleistocene coral reefs associated with claystones, southwestern Taiwan

S. Y. Gong, S. W. Wang, Tung-Yi Lee

    Research output: Contribution to journalArticlepeer-review

    8 Citations (Scopus)


    Scleractinian coral reefs, when coexistent with siliciclastic sediments, usually occur in association with deltaic or coastal sands. Nevertheless, Pleistocene reef limestones in southwestern Taiwan are developed in association with thick claystones that were deposited in a deeper-water environment. These reef limestones are characterized by: (1) rapid transition from underlying claystones upward to reefal limestones, (2) lateral interfingering with open-shelf claystones, (3) being overlain by terrestrial deposits or exposed with no covering strata, and (4) being located in close association with anticlines. The authors propose that these reef limestones developed on anticlinal ridges raised above the adjacent sea floor by thrust-front migration in a foreland setting.

    Original languageEnglish
    Pages (from-to)215-222
    Number of pages8
    JournalCoral Reefs
    Issue number3
    Publication statusPublished - 1998 Sep 1


    • Coral reefs
    • Foreland wasin
    • Pleistocene
    • Siliciclastics
    • Taiwan
    • Tectonic control

    ASJC Scopus subject areas

    • Aquatic Science

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