东海陆架盆地N气田花港组储层特征及分类评价
东海陆架盆地N气田花港组储层特征及分类评价
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Beijing: Marine Geology and Quaternary Geology
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Chinese
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Beijing: Marine Geology and Quaternary Geology
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Contents
东海陆架盆地西湖凹陷古近系花港组储层为典型的低孔、低渗储层。基于大量岩心物性、粒度、薄片、压汞等资料,对N气田目的层储层岩性、物性和孔隙结构特征进行精细评价。结果表明:N气田花港组储层岩性以细砂岩为主,矿物成分构成稳定,以石英为主,黏土含量低,岩性较纯;随着埋藏变深,孔隙变差,粒间孔减少,溶蚀孔增加,孔喉半径减小,连通性变差;局部发育砂砾岩,且渗透率大于细砂岩一个数量级以上,可作为甜点储层开发。基于实验和试油资料统计结果,建立了一套适用于花港组储层的综合分类评价标准,包含孔隙度、渗透率、饱和度和地质特征4类储层重要参数,分类结果特征鲜明,分类依据科学可靠,为该区域低孔、低渗储层勘探开发提供依据。
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东海陆架盆地N气田花港组储层特征及分类评价
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TN_cdi_wanfang_journals_hydzydsjdz202102017
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https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_wanfang_journals_hydzydsjdz202102017
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ISSN
0256-1492
DOI
10.16562/j.cnki.0256-1492.2020061203