【摘要】 风暴岩自1973年G.Kelling提出以来,其研究得以迅速发展,特别是建立的风暴流理论与50年代出现的浊流理论一样,被公认为沉积学乃至地质学发展的里程碑。本文回顾了国内外风暴岩研究的历程、现状,着重综述了国内外对风暴岩研究的起源、定义,及风暴岩的沉积成因、沉积序列、沉积构造和研究意义;分析了风暴岩的形成环境和研究尺度,对未来风暴岩研究的启示,并探讨了兴文风暴岩研究对兴文世界地质公园的意义。更多还原

【Abstract】 Since G.Kelling put forward tempestite in 1973,the study of it,especially the storm flow theory to be known to be a milestone of development of sedimentology and even geology,has made considerable advances.This paper gives a review of history and present situation of the study of tempestite at home and abroad,especially,definition,sedimentary sequence,sedimentary structure and theoretical and practical significance and makes an approach to sedimentary environment of tempestite and significance of the study of tempestite to the Xingwen World Geopark.更多还原