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- W2365005374 abstract "The Pipe-Rocks or burrows Skolithos studied here are found in Lingqiu County, Shanxzi Province, North China. They are as abundant and magnificent as ones from other famous localities in the world. The burrows Skolithos reported here occur in a set of clastic rocks dominated by the red sandstone, which were compared to the Neoproterozoic Qingbaikou System (1 000 800 Ma) in Yanshan Range previously. In this paper they are built a new formation, the Yuncailing Formation. It is disconformably overlain by the Maozhuang Formation of the Lower Cambrian and overlies the Wumishan or Gaoyuzhuang Formation of the Middle Proterozoic unconformably, with a thickness from some meters to more than 100 meters. The Pipe rocks or burrows are c.5~20 m thicken and occurs in the middle part of the Yunca iling formation. Based on their diagnosis, these burrows are well compared with Skolithos linearis Haldeman that is distributed in the Lower Cambrian. On the basis of studying and comparing results mentioned above, the burrow-bearing sequence of clastic rocks, i.e. Yuncailing Formation, should be assigned to the lower Cambrian and not the Neoproterozoic Qingbaikou System. Because the Yuncailing Formation underlies the Chanping Formation (or Fujunshan Formation) belonging to the early stage of the Early Cambrian in adjacent area, it means that this burrow bearing sequence will be the lowerest Cambrian rocks in the North China Platform possibly. Based on the presence of the Skolithos and other available depositional marks, it seems that the Yuncailing Formation was formed in the palaeoenvironment of delta facies." @default.
- W2365005374 created "2016-06-24" @default.
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- W2365005374 date "2001-01-01" @default.
- W2365005374 modified "2023-09-25" @default.
- W2365005374 title "Pipe-Rocks-Skolithos from Lingqiu County of Shanxi Province, China" @default.
- W2365005374 hasPublicationYear "2001" @default.
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