录井工程 ›› 2022, Vol. 33 ›› Issue (4): 112-117.doi: 10.3969/j.issn.1672-9803.2022.04.019
艾笛①, 姚亚彬②, 芮昀②, 魏宝军③, 郭宁①, 丁邦春④
AI Di①, YAO Yabin①, RUI Yun②, WEI Baojun③, GUO Ning①, DING Bangchun④
摘要: 溶蚀孔洞是滇黔北坳陷灯影组碳酸盐岩的主要储集空间,为了研究碳酸盐岩的岩溶发育规律及测井响应特征,综合利用岩心、薄片、常规测井和电成像资料分析了区内岩溶的地质特征和测井响应特征,在此基础上自上而下将岩溶层划分为垂直渗流岩溶带和水平潜流岩溶带,并对其分布规律进行了研究。结果表明,滇黔北坳陷岩溶发育受古地貌影响大,岩溶坡地岩溶发育程度高,其中溶缝、溶洞、溶孔发育,可作为有效储集空间,进而通过在横向上与川中高石梯-磨溪地区加以对比,揭示了该区岩溶地层勘探潜力,为精细评价该区储层奠定了基础,对下一步油气勘探决策具有良好的指导意义。
中图分类号:
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