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台湾地层以台湾山脉东坡的晚古生界至中生界为基底,向台湾西部地区时代逐渐变新.台湾东部的台东山脉地层属一时代较新的独特地块.台湾本岛主要的地层都为一向西凸出的长弧形,呈大致和台湾岛长轴平行
The Taiwan strata, based on the Late Paleozoic to the Mesozoic in the eastern slope of Taiwan’s mountain range, are gradually becoming new in the era of Taiwan’s western region.The Taitung Mountain Range in the eastern part of Taiwan is a newer and more unique parcel of land.Taiwan’s main strata They are all long arcs that protrude westwards and are generally parallel to the axis of Taiwan’s island