北京中生代地层及生物群研究
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THE MESOZOIC STRATIGRAPHY AND BIOTA OF THE BEIJING AREA
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    摘要:

    在前人研究的基础上,我们对北京地区中生代地层和生物群进行了研究。依植物化石资料与岩性对比,肯定了三叠系的存在。上统含拟丹尼蕨等晚三叠世标准化石,时代明确;中统未见化石;下统含二叠—三叠纪过渡性化石,时代归属有争议。侏罗系在北京地区分布广、厚度大、矿产丰富、沉积类型复杂。文中从动、植物化石组合,岩相与火山活动等多方面做了新的探讨。白垩系出露面积很小,属断陷盆地沉积,但化石极丰富,含标准的热河生物群及与之有演替关系的房山生物群分子;另对盆地的地质演化历程也有简单叙述。

    Abstract:

    The Mesozoic is very important to the geological research in the Beijingarea, because it has a widespread distribution and a huge thickness, is a typicalvolcano-sedimentary sequence, has a tectonic setting involving the Indo-sinianand Yanshanian movements, experienced frequent magmatism, and is character-ized by rapid biotic evolution, a varity of fossil groups and abundant mineralresources. The study on the Mesozoic stratigraphy and biota is of great impor-tance both iu theory and in practice. The Triassic in the Beijing area, also known as the shuangquan Group, in-cludes three formations: Dabeisi, Tanzhesi and Xingshikou. Of the Mesozoic in the Beijing area, the Jurassic sequence is the thickest,most widespread, richest in plant fossils and most complicated in sediment types.It includes 3 series, 2 groups and 9 formations. The Cretaceous in the Beijing area is exposed in the Tuoli-Dahuichang vic-inity, covering an area of some 200 km~2. It includes 2 groups and 6 formations,yielding abundant animal and plant fossils. The area is one of the famous LateMesozoic down-faulted basins in North China.

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萧宗正,杨鸿连,单青生.1993.北京中生代地层及生物群研究[J].地质论评,39(5):442-450,[DOI].
Xiao Zongzheng, Yang Honglian, Shan Qingsheng Geological Institute of Beijing, Beijing.1993. THE MESOZOIC STRATIGRAPHY AND BIOTA OF THE BEIJING AREA[J]. Geological Review,39(5):442-450.

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