东海某凹陷平北区基底岩浆岩优质储层发育模式

苗清, 张武, 赵幸滨, 肖晓光, 李峻颉. 东海某凹陷平北区基底岩浆岩优质储层发育模式[J]. 海洋地质与第四纪地质, 2019, 39(6): 93-101. doi: 10.16562/j.cnki.0256-1492.2019070502
引用本文: 苗清, 张武, 赵幸滨, 肖晓光, 李峻颉. 东海某凹陷平北区基底岩浆岩优质储层发育模式[J]. 海洋地质与第四纪地质, 2019, 39(6): 93-101. doi: 10.16562/j.cnki.0256-1492.2019070502
MIAO Qing, ZHANG Wu, ZHAO Xingbin, XIAO Xiaoguang, LI Junjie. The development model for high quality magmatic basement reservoir in a depression of East China Sea[J]. Marine Geology & Quaternary Geology, 2019, 39(6): 93-101. doi: 10.16562/j.cnki.0256-1492.2019070502
Citation: MIAO Qing, ZHANG Wu, ZHAO Xingbin, XIAO Xiaoguang, LI Junjie. The development model for high quality magmatic basement reservoir in a depression of East China Sea[J]. Marine Geology & Quaternary Geology, 2019, 39(6): 93-101. doi: 10.16562/j.cnki.0256-1492.2019070502

东海某凹陷平北区基底岩浆岩优质储层发育模式

  • 基金项目: “十三五”国家科技重大专项“深层优势储层孔喉结构及成岩环境分析技术”(2016ZX05027-002)
详细信息
    作者简介: 苗清(1988—),女,硕士,工程师,主要从事沉积储层研究,E-mail: miaoqing5@cnooc.com.cn
  • 中图分类号: P744.4

The development model for high quality magmatic basement reservoir in a depression of East China Sea

  • 综合利用岩心、薄片、压汞数据、测井曲线及储层物性等资料,对平北地区基底岩浆岩储层特征及优质储层发育条件等进行研究。结果表明,储层以花岗岩储层物性最好,其储集空间以构造缝、溶蚀缝和溶蚀孔为主,其中,构造缝占比61%,在作为良好的储集空间的同时,也为原生孔隙的连通起到至关重要的作用。本区花岗岩储层发育具Ⅰ型模式,即,整体呈漏斗形,上部地区因裂缝、溶蚀孔洞被充填而形成致密区,储层物性差;中部大气淡水淋滤和构造应力作用下,裂缝发育,具备优异的储集空间和孔喉条件,为优质储层发育区;下部大气淡水淋滤作用弱,构造应力影响小,裂缝不发育,储层物性最差。研究认为优质基底岩浆岩储层位于基底中上部,大气淡水淋滤作用强,构造应力强,断层、断裂较为发育的地区。

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  • 图 1  东海某凹陷平北地区位置图

    Figure 1. 

    图 2  平北区基底岩浆岩镜下特征

    Figure 2. 

    图 10 

    图 3  东海陆架盆地新生界基底岩性及构造区划图(据徐发2012,有修改;框内为研究区)

    Figure 3. 

    图 4  A3井基底花岗岩次生孔隙特征

    Figure 4. 

    图 5  A3井基底花岗岩裂缝特征

    Figure 5. 

    图 6  平湖构造带A3井储层风化溶蚀及裂缝发育特征

    Figure 6. 

    图 7  储层岩石类型与物性特征(汞饱和度和毛管压力、孔喉半径的关系)

    Figure 7. 

    图 8  A3井Ⅰ型储层发育模式

    Figure 8. 

    图 9  平北区基底潜山优质储层发育模式

    Figure 9. 

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出版历程
收稿日期:  2019-07-05
修回日期:  2019-08-26
刊出日期:  2019-12-25

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