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Late Quaternary formation of the Miaoli Tableland in northwest Taiwan, an interplay of tectonic uplift and fluvial processes dated by OSL

Datos Bibliográficos

ID24088262
AutoresShih-Hung Liu (0000-0001-5986-7985, Freie Universität Berlin, autor de correspondencia), Christopher Lüthgens (0000-0003-3211-6318, BOKU University), Jacob Hardt (0000-0001-8485-2232, Freie Universität Berlin), Robert Hebenstreit (0000-0002-5941-6196, Freie Universität Berlin), Martina Böse (0000-0002-7454-0072, Freie Universität Berlin), Margot Böse, Manfred Frechen (LIAG Institute for Applied Geophysics)
Año2023
Volumen112
Páginas128-149
Fecha de publicación2023-03-01
Peer ReviewedSí
Open AccessSí
TipoARTICLE
RevistaQuaternary Research (JOURNAL)
Identificadores de la revistaISSN: 0033-5894 • E-ISSN: 1096-0287
EditorialCambridge University Press (CUP) (PUBLISHER)
DOI10.1017/qua.2022.52
OpenAlexW4311106458
IdiomaEN
Referencias citadas87

The “tablelands” in Taiwan are sedimentary terraces occurring in the foreland basin west of the Neogene mountain ranges. The Miaoli Tableland consists of elevated Late Quaternary sedimentary successions, representing a change from tidal to coastal and fluvial to eolian depositional environments. The present-day morphology is a result of combined processes, including differential tectonic uplift, ongoing fluvial aggradation, and incision. Selected deposits in 10 outcrops were sampled and studied by optical dating. The deposition of fluvial sediments started after the last interglacial (

Aggradation · Fluvial · Foreland basin · Geochemistry · Geomorphology · Quaternary · Sedimentary depositional environment · Sedimentary rock · Structural basin · Tectonic uplift · Tectonics · Geological formations and processes · Geology · Geology and Paleoclimatology Research · Methane Hydrates and Related Phenomena · Paleontology

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