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利用地震属性分析沉积环境的误区:以辽河盆地滩海东部凹陷东二段为例
Pitfall in sedimentary interpretation using seismic attributes:An example from Dong2 member in East Depression,offshore area of Liaohe Basin
【摘要】 为了解辽河盆地滩海地区东二段沉积相类型,通过现代河流沉积调研以及岩心、测井、地震相综合分析,结果证明:滩海地区东二段沉积相类型主要以滨浅湖-滩坝相为主,而非地震属性图所反映的河流相沉积,地震属性解释存在误区。古沉积环境解释最重要的因素就是如何理解"保存"的概念。河流在自身演化过程中迁移、改道时常发生,在漫长的地质时间内,难以保存一个完整的河道。沉积环境分析中,应当遵循从岩心相—测井相—地震相的分析过程,而不是单纯依据地震属性直接进行沉积相研究。
【Abstract】 To better understand sedimentary types in the Dong2member of offshore in the Liaohe Basin,through the research of modern river deposition and comprehensive analyses of cores,well logs,and seismic profiles,it was proved that the dominant facies in Dong2member is characterized by shore shallow lacustrine-beach-bar facies,instead of the fluvial facies deduced by seismic attributes slices.The key factor in interpreting ancient depositional environment is the concept of"preservation".Migration and divagation often happened during the river evolution,so it is hard to preserve a complete river channel.Analyses of the sedimentary environments should follow the study order of core facies-logging facies-seismic facies,but not only based on seismic attributes.
【Key words】 seismic attributes; Dong 2Member; fluvial sediment; beach-bar; offshore;
- 【文献出处】 地学前缘 ,Earth Science Frontiers , 编辑部邮箱 ,2012年01期
- 【分类号】P618.13;P631.4
- 【被引频次】4
- 【下载频次】381