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- W2020543905 abstract "Collision between the Philippine Plate and the Eurasian Plate has caused recent tectonics in the southwestern alluvial plain of Taiwan. A fold, which is the near-surface evidence of this recent tectonics, has been found using a shallow seismic method. The fold passes through 23°13.83′N and 120°07.54′E and strikes about N10W. Nearly parallel to the Taiwan Strait coastline, the fold is only a few kilometres away. The fold is in unconsolidated sediments and is possibly an extension of a blind thrust fault. Folding of near-surface strata suggests deformation within the last 10 ka, consistent with the proposition of Biq (Ti-Chi 12 (1992) 1–12) that the recent Taiwan Orogeny is at its early stage. This recent tectonics also provides evidence that the plate boundary in Taiwan is migrating northwestward." @default.
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- W2020543905 date "1998-11-01" @default.
- W2020543905 modified "2023-09-24" @default.
- W2020543905 title "Near-surface evidence of recent Taiwan Orogeny detected by a shallow seismic method" @default.
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- W2020543905 doi "https://doi.org/10.1016/s0012-821x(98)00194-0" @default.
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