吉林大学学报(地球科学版) ›› 2018, Vol. 48 ›› Issue (4): 965-980.doi: 10.13278/j.cnki.jjuese.20170082
陈爱民
Chen Aimin
摘要: Bonaparte盆地属于陆内裂谷与被动大陆边缘相叠加的叠合型盆地,WA-406-P区块就位于盆地早-中侏罗世发育的大型Plover三角洲沉积体系之上,该区块油气成藏条件及控制因素的研究是确定下步有利勘探目标的前提与基础。本文结合油气地质、分析化验、三维地震、测井曲线等资料进行综合分析,研究表明:WA-406-P区块发育两种烃源岩类型,西北部以Ⅱ1型为主,东南部以Ⅱ2型为主,成岩作用控制着储层的储集性能,整体上属于低孔高渗透型储层;中-下侏罗统的Plover组和Elang组及上侏罗统-下白垩统的Flamingo组三套三角洲砂体与大套的海相泥岩配置形成两套有利储盖组合,由于圈闭形成期早于大规模油气运聚期,因此,油气经历两期充注后,具备良好的成藏匹配关系。烃源岩分布特征控制着油气藏的流体类型,构造形态及断层展布控制着油气藏的类型,储层物性控制着油气地质储量的丰度,断层活化作用控制着油气藏能否完整保存。油气成藏控制作用的明确指明了有利勘探区域:北部垒堑间互带为Ⅰ类勘探区,西南斜坡带为Ⅱ类勘探区,东南洼槽区为Ⅲ类勘探区。
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