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本文总结了风暴沉积特征与基本风暴事件沉积类型,并比较了风暴、浊流、洪水事件沉积异同。通过对塔里木盆地巴楚达板塔格上寒武—下奥陶统剖面实测,于鹰山组上部发现风暴岩沉积序列。对该风暴沉积序列的沉积特征与沉积环境作了研究,初步认为其代表了浪基面与风暴浪基面间下部环境的沉积。
This paper summarizes the sedimentation characteristics of storm deposits and the basic storm events and compares the similarities and differences of storm, turbidity and flood events. By measuring the Upper Cambrian-Lower Ordovician section of Bangtag in Batiuda, Tarim Basin, the sedimentary sequences of storm rocks are found in the upper part of Yingshan Formation. The sedimentary characteristics and sedimentary environment of the sedimentary sequence of the storm are studied, and it is preliminarily considered that it represents the deposition of the lower environment between the wave basal plane and the storm wave basal plane.