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自八十年代-九十年初一些地质时代表(Haq等,1988;Cowic和Bassett,1989;Odin和Odin,1990;Harland等,1990)发表以来,已取得了相当多的新资料和更详细的磁性地层和生物地层资料。由F.M.Gradstein和Ogg编制的显生宙地质时代表汇集了最近的地质时代信息。其中新生代时代表依据Berggren等(1995)和Hilgen(1991〕,中生代时代表依据Gradstein等(1995),古生代时代表据Harland等(1990)并对前石炭纪根据Ro—berts等(1995)和Tucker与Mckerrow(1995)的更精确的期界线的同位素年代作了修改。 这一新的显生宙地质时代表发表于国际地质科学联合会出版的国际地质科学新闻杂志《Episodes》的1996年3—6月的Vol.19,No.1—2。现转载供读者参考(原图为彩色图)。
Since the publication of some geologic timepieces of the 1980s-early 1990s (Haq et al., 1988; Cowic and Bassett, 1989; Odin and Odin, 1990; Harland et al., 1990), considerable new information has been obtained and more detailed Magnetic stratum and biostratigraphic data. The Phanerozoic geologic time series compiled by F.M. Gradstein and Ogg brings together recent geological information. According to Bergsren et al. (1995) and Hilgen (1991), Mesozoic epochs are based on Gradstein et al. (1995) and Paleozoic epochs according to Harland et al. (1990) Tucker and Mckerrow (1995) revised the more precise period of the isotopic dating of this new Phanerozoic geology published in the International Journal of Geological Science published by the International Journal of Geological Science “Episodes” in 1996 3 - June Vol.19, No. 1-2. Reprint for readers reference (the original color chart).