• 责任者：Yang Hongjun (Zhanjiang Branch Company ; CNOOC ; Zhanjiang 524057 ; China) ; Guo Shusheng
• 刊名：Petroleum Geology & Experiment
• 出版年：2013
• 卷期：35(6)
• 关键词：重力流 ; gravity flows ; 沉积构造 ; sedimentary structure ; 莺歌海盆地 ; Yinggehai Basin
• 页码：p.626-633
• 图表：4 illus., 24 refs.
• 分类号：0803
• issnNo：ISSN1001-6112
• isbnNo：CN32-1151/TE

     Integrated with cores, micro-resistivity images and conventional logs, deposits in the 1st member of the Huangliu Formation of the Upper Miocene in the SY and SE areas in the Dongfang tectonic belt of the Yinggehai Basin were analyzed in detail. It was shown that a set of fine-grained deposits of submarine fan deve- loped in the 1 st member of the Huangliu Formation, and the deposits were reformed by internal wave and internal tide of deep-water tract current during gravity flow deposition process, forming 5 typical lithofacies： 1 ） finekinds of deposits coupled locally.