丽水-椒江凹陷古新统不同物源下沉积体系储层品质研究及优选

    A comparative study on reservoir quality of different Paleocene depositional systems in the Lishui-Jiaojiang Sag

    • 摘要: 丽水-椒江凹陷作为古新统断陷盆地,在分区供源背景下的不同沉积体系储层品质差异较大。为厘清不同沉积体系下的优质储层成因并寻找有利勘探目标,本研究应用岩芯、测井、地震及分析化验资料,对凹陷内的沉积体系进行识别,并对相同砂岩类型、相近埋深条件的不同沉积体系储层品质进行对比分析。结果表明,丽水B洼发育浙闽隆起南部供源的浅海海底扇和滩坝两类沉积体系,砂岩类型以富含火山岩屑的岩屑砂岩为主。相近埋深下,滩坝砂体经强水动力的反复淘洗,颗粒磨圆分选较好,塑形火山岩屑含量低,结构和成分成熟度较高,储层品质优于浅海海底扇砂体。丽水A洼、C洼和椒江凹陷发育浙闽隆起北部和雁荡凸起供源的辫状河三角洲和扇三角洲沉积体系,储层变质岩岩屑及长英质颗粒含量较高,抗压能力强,物性整体较好。相近埋深的辫状河三角洲前缘近端和扇三角洲前缘近端砂砾岩及粗砂岩储层品质整体优于前缘远端细砂岩,粒度为该区优质储层主控因素。因此,在丽水B洼可针对具备较高成熟度的滩坝以及浅海海底扇近端叠置水道和水道席状砂复合砂体进行优先勘探;在丽水A洼、C洼和椒江凹陷,辫状河三角洲和扇三角洲的前缘近端以及发育强水动力粗粒甜点的远端具备较好的储层品质和较大的勘探潜力。

       

      Abstract: The Lishui-Jiaojiang Sag, a Paleocene rift basin, varies significantly in reservoir quality among different depositional systems of multiple provenances. To characterize the reservoirs of various depositional systems and identify favorable exploration prospects, we integrated data from cores, well logs, seismic surveys, and laboratory analyses to identify various depositional systems and compare reservoir quality of similar sandstone types and burial depths. Results show that the Lishui Sub-sag B developed two depositional systems in the Cenozoic: shallow-marine submarine fans and sand bars, and they both originated in the southern Zhemin Uplift. The sandstone types are predominantly litharenite rich in volcanic lithics. At similar burial depths, sand bars are under strong hydrodynamic conditions and repeated winnowing, resulting in better grain roundness and sorting, lower content of plastic volcanic lithics, and consequently superior reservoir quality compared to those of submarine fans. In the Lishui Sub-sag A, Sub-sag C, and Jiaojiang Sag, braided delta and fan delta depositional systems were developed, from the source areas of northern Zhemin Uplift and the Yandang Uplift. The reservoirs are characterized by relatively high porosity and permeability, due to higher contents of metamorphic lithics and felsic minerals that are resistant to mechanical compaction. Under similar burial depths, the reservoir quality of conglomerates and coarse-grained sandstone in the proximal braided delta fronts and fan delta fronts is significantly better than that of fine-grained sandstone in distal delta front settings. Grain size is the pivotal factor for high-quality reservoirs in this region. Therefore, we recommended that in the Lishui Sub-sag B, priority exploration shall be directed to sand bars and amalgamated channels and channelized lobes in proximal submarine fans and relatively high maturity. In the Lishui Sub-sag A, Sub-sag C, and Jiaojiang Sag, the proximal delta front areas, along with distal high-energy coarse-grained “sweet spots”, have superior reservoir quality and hold promising exploration potential.

       

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