Holocene tectonic uplift deduced from elevated shorelines, eastern Coastal Range of Taiwan

This paper is concerned with the tectonic trends that can be deduced from the Holocene raised shorelines between Ch'eng-kung and Hsin-she, along a 65-km long coastal sector in the eastern Coastal Range of Taiwan. Sequences of up to eight superimposed shorelines have been identified in a single...

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Published inTectonophysics Vol. 222; no. 1; pp. 55 - 68
Main Authors Liew, P.M., Pirazzoli, P.A., Hsieh, M.L., Arnold, M., Barusseau, J.P., Fontugne, M., Giresse, P.
Format Journal Article
LanguageEnglish
Published London Elsevier B.V 15.06.1993
Amsterdam Elsevier Science
New York, NY Elsevier
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Summary:This paper is concerned with the tectonic trends that can be deduced from the Holocene raised shorelines between Ch'eng-kung and Hsin-she, along a 65-km long coastal sector in the eastern Coastal Range of Taiwan. Sequences of up to eight superimposed shorelines have been identified in a single section. Twelve new radiocarbon dates (six of which were obtained by accelerator mass spectrometry) of in-situ marine samples (up to 40 m in altitude) have confirmed a Holocene age. However, it is difficult to define clearly the upper marine boundary in the highest Holocene coastal terraces, which have been uplifted to 65–70 m, but have been capped by, and often also interfingered with, alluvial deposits. High uplift rates, ranging from 2.5–3.0 to over 8 mm/yr, have been inferred along the coast, providing evidence of differential uplift. In some cases uplift movements appear to have occurred by steps, probably spasmodically. Recurrence periods of fast uplifts seem to be of the order of at most 1000 yr. This means that a new spasmodic movement may be imminent, because the last displacement (4–6 m) has been dated about 1000 yr BP.
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content type line 23
ISSN:0040-1951
1879-3266
DOI:10.1016/0040-1951(93)90189-Q