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在开放的陆架环境中,风暴沉积是一种常见的事件沉积,但在古代和现代的风暴沉积中,却很难发现保存完整的风暴沉积序列,其原因是风暴沉积的结构构造非常容易受到后来的机械作用的改造和生物扰动的破坏。幸运的是,山东省寒武系崮山组上部的薄层灰岩不仅比较完整地保存了风暴成因的机械作用结构、构造,同时,也详尽地记录了与风暴成因有关的生物成因的沉积构造。根据崮山组薄层灰岩中保存的风暴成因沉积序列和前人所总结的风暴沉积模式,可以建立一个理想的综合性的风暴沉积—正常气候条件下包括机械作用和生物作用的沉积序列,这对于解释风暴作用的整个过程,鉴别现代的或古代的不同沉积环境的风暴沉积,在理论上和实践中均具有重要意义。风暴沉积与浊流沉积的区别在于前者具有浅水的生物群和不同的机械成因的和生物成因的沉积构造。
Storm deposits are a common event deposit in an open shelf environment, but the preservation of intact storm deposits is difficult to find in ancient and modern storm deposits because the structural formation of the storm deposits is highly susceptible to later The mechanical effects of the transformation and the destruction of biological disturbance. Fortunately, the thin-bedded limestone in the upper part of the Dangshan Formation in the Cambrian of Shandong Province not only completely preserved the mechanistic structure and structure of the storm, but also recorded in detail the sedimentary structures of the biogenic origin related to the genesis of the storm . According to the sequence of storm deposits deposited in the thin-layer limestone of the Jushan Formation and the storm deposition patterns previously summarized, it is possible to establish a comprehensive and comprehensive storm sediment deposition sequence, including mechanical and biological processes under normal climatic conditions, This is of great significance both theoretically and practically for the whole process of explaining the storm effect and for identifying storm deposits in modern or ancient sedimentary environments. The difference between storm deposits and turbidity flows is that the former has a shallow water biota and different mechanistic and biogenic sedimentary formations.