珠江口盆地陆丰地区恩平组层序地层控制的河道构成样式
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摘要
依据河流相层序地层理论,综合利用岩心、测井以及地震资料,开展了陆丰地区恩平组不同层序地层位置河道构成解剖工作,将恩平组划分为3个受可容纳空间变化控制的三级层序,提出了低可容纳空间条件下形成的厚层—叠置的三角洲平原辫状分流河道、中等可容纳空间条件下形成的厚层、叠置—孤立三角洲前缘分支河道以及高可容纳空间条件下形成的薄层、朵叶体上孤立分支河道—席状砂3种不同河道构成样式。不同构成样式河道的油藏特征具有明显的差异。其中,低可容纳空间条件下形成的厚层—叠置的三角洲平原辫状分流河道以构造油气藏为主,高可容纳空间条件下形成的薄层、朵叶体上孤立分支河道以岩性油气藏为主。该分析方法、手段在其他类似地区具有一定的借鉴意义。
Based on the integrated utilization of cores,logging and seismic data,and according to the fluvial sequence stratigraphic theory,the channel stacking patterns of Enping Formation were analyzed.Enping Formation was divided into three 3 rd-order sequences which were controlled by the variation of accommodation.The three channel stacking patterns were summarized:Thick-stacked delta plain braided distributary channels under low accommodation,thick-stacked or isolated delta front branch channels under middle accommodation,thin-isolated branch channels-sheet sand under high accommodation.Different channel stacking patterns have different reservoir characteristics.The thick-stacked delta plain braided distributary channels under low accommodation mainly formed structural reservoirs,and the thin-isolated branch channels-sheet sand under high accommodation mainly formed lithologic reservoirs.This analysis method has some reference significance for other similar areas.
Based on the integrated utilization of cores,logging and seismic data,and according to the fluvial sequence stratigraphic theory,the channel stacking patterns of Enping Formation were analyzed.Enping Formation was divided into three 3 rd-order sequences which were controlled by the variation of accommodation.The three channel stacking patterns were summarized:Thick-stacked delta plain braided distributary channels under low accommodation,thick-stacked or isolated delta front branch channels under middle accommodation,thin-isolated branch channels-sheet sand under high accommodation.Different channel stacking patterns have different reservoir characteristics.The thick-stacked delta plain braided distributary channels under low accommodation mainly formed structural reservoirs,and the thin-isolated branch channels-sheet sand under high accommodation mainly formed lithologic reservoirs.This analysis method has some reference significance for other similar areas.
引文
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