首页> 外文会议>International Symposium on the Cambrian System >EDIACARAN-CAMBRIAN BOUNDARY SECTIONS AND EARLY CAMBRIAN CHENGJIANG NONMINERALIZED FOSSILS IN EASTERN YUNNAN PROVINCE, SOUTHWESTERN CHINA: INTRODUCTION
【24h】

EDIACARAN-CAMBRIAN BOUNDARY SECTIONS AND EARLY CAMBRIAN CHENGJIANG NONMINERALIZED FOSSILS IN EASTERN YUNNAN PROVINCE, SOUTHWESTERN CHINA: INTRODUCTION

机译:Ediacaran-Cambrian边界和云南东部云南省东部的寒武纪诚江非崩江非崩新化石:介绍

获取原文

摘要

Eastern Yunnan lies on the southwestern margin of the Yangtze Platform, South China. Lower Cambrian strata are extensively developed and well exposed in the area (Fig. 1). Since the beginning of the last century (Depret, 1912), eastern Yunnan has been a special place for the study on the Neoproterozoic-lower Cambrian in China (Zhu et al., 2001), because of the following reasons: 1, the presence of well developed, well exposed Lower Cambrian strata containing the most complete sequence of lower Cambrian shallow-water environments in China; and 2, the presence of abundant fossils recording a clear succession of Early Cambrian communities.
机译:云南东部位于华南长江平台的西南边缘。下寒册地层广泛开发并在该区域中暴露良好(图1)。自上世纪初(1912年)开始以来,云南东部是在中国新典型乔治尼亚下寒武纪的研究(Zhu等,2001),因为以下原因:1,存在开发良好,暴露良好的下部寒夜地层,含有最完整的中国较低的下寒柬浅水环境序列; 2,存在丰富的化石,记录清晰的早期寒武纪社区。

著录项

相似文献

  • 外文文献
  • 中文文献
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号