豫西卢氏县朱阳关组的建立

    THE ESTABLISHMENT OF THE ZHUYANGGUAN FORMATION

    • 摘要: 在河南省卢氏县朱阳关一带,发育一套陆相碎屑岩建造,具有一定的厚度和展布范围,上下界线清楚,为一独立的岩石地层单位,代表北秦岭地层分区晚白垩世地层沉积。过去未曾有人对该套地层命名,经研究,认为符合建组条件,故将其建组,命名为朱阳关组。本文还对朱阳关组层型剖面进行了介绍。

       

      Abstract: In the vicinity of Zhuyangguan,Lushi county,Henan province,there occurs a sequence of terrestrial clasticrocks. With a certain thickness,distribution extent and clear boundaries, it is an independent lithostratigraphic unit,representing Late Cretaceous sediments in the northern Qinling stratigraphic area. In the past this sequence was notnamed by anyone. Studies show that it meets requirements for establishing a formation,so it is designated as a for-mation named the Zhuyangguan Formtion.This paper also introduced the stratotype section of the ZhyangguanFormation.

       

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