The sequence boundaries and the slope-break zones are the important factors to control creation of stratigraphic and lithologic traps in the area.
层序地层边界和坡折带是控制本区地层岩性圈闭形成的重要因素。
The sequence boundaries and the slope-break zones are the important factors to control creation of stratigraphic and lithologic traps in the area.
层序地层边界和坡折带是控制本区地层岩性圈闭形成的重要因素。
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