论文部分内容阅读
浙江绍兴漓渚地区寒武、奥陶系发育较好,大致呈狭长条带自漓渚附近往西南延伸至诸暨江藻,因第四系掩盖和断层切割,分布不甚连续。1980年9月和12月笔者在区内测制剖面,采集各门类化石五百余块。依据剖面及化石将本区寒武系划分为五组,奥陶系划分为六组。何家山头剖面是这次所测寒武、奥陶系的主要剖面。柁山坞剖面是增补化石的辅助剖面。谢坞、棠棣和朱家站三个分界剖面分别补充何家山头剖面未见寒武系底
The Cambrian and Ordovician in Shazhu, Lixia, Shaoxing, Zhejiang Province developed well, with a narrow strip extending from the vicinity of the LiZhuZhu to the Zhuji River and algae in southwestern China. Due to the cover of the Quaternary and the fault cutting, the distribution was not continuous. In September 1980 and December 1980, the author made profiles in the area and collected more than 500 pieces of various fossils. Based on the profiles and fossils, the Cambrian of the area is divided into five groups, and Ordovician is divided into six groups. Ho Hill section is measured by the Cambrian, Ordovician Department of the main profile.柁 Hill dock section is supplementary fossil profile. Xie dock, Tong Di and Zhu station three sections were added to the Ho Ka Shan head section no Cambrian Department