地学前缘 ›› 2018, Vol. 25 ›› Issue (2): 92-98.DOI: 10.13745/j.esf.2018.02.010

• 沉积相与储层 • 上一篇    下一篇

多信息关联的辫状河储层夹层预测方法研究:以南苏丹P油田Fal块为例

王敏,穆龙新,赵国良,客伟利,邹荃,康楚娟   

  1. 中国石油勘探开发研究院, 北京 100083
  • 收稿日期:2017-09-10 修回日期:2017-10-20 出版日期:2018-03-15 发布日期:2018-03-15
  • 作者简介:王敏(1981—),女,博士,工程师,主要从事油气田开发地质研究工作。E-mail:wangmin1604@petrochina.com.cn
  • 基金资助:
    中国石油天然气集团公司重大专项“南苏丹3/7区大型层状砂岩油藏控水稳油综合调整研究”(2016D-4401)

Multiinformation association for interlayer prediction in braided river reservoir: taking Fal Structure of P field, South Sudan as an example.

WANG Min,MU Longxin,ZHAO Guoliang,KE Weili,ZOU Quan,KANG Chujuan   

  1. PetroChina Research Institute of Petroleum Exploration & Development, Beijing 100083, China
  • Received:2017-09-10 Revised:2017-10-20 Online:2018-03-15 Published:2018-03-15

摘要: 辫状河储层的夹层预测是油藏描述的重点内容。目前夹层的预测主要集中于夹层发育模式研究和心滩坝体的构型单元解剖,且多运用单一的预测方法。南苏丹P油田辫状河储层夹层类型多、规模差异大、分布复杂,定量表征难度较大,在文献调研的基础上,从夹层的沉积成因入手,依据不同沉积方式形成的沉积砂体及其内部泥质夹层形态与结构不同的特点,综合岩心、测井与地震等多种资料,提出多信息关联的辫状河储层夹层预测方法。在密井网区建立骨架剖面与三角网小剖面,运用测井资料的垂向高分辨率与地震资料的横向强连续性特征确定不同类型夹层的井间发育规模;在建立岩相模型的基础上,以隔层厚度分布图为约束条件,采用确定性建模方法建立稳定泥岩隔层分布模型;以沉积微相研究结果和夹层规模预测结果为约束条件,采用随机建模方法分别在砂岩相和泥岩非隔层相中模拟心滩坝、河道和各类型夹层的分布;最终确定了研究区主要存在4种成因类型的夹层,并在多信息关联的基础上建立反映多类型夹层空间分布的辫状河储层精细地质模型。研究发现,对于厚度大于2 m的夹层可以通过井震结合的方法验证其井间规模,定量确定不同层位、不同类型夹层顺物源与切物源的发育规模,为夹层模型的建立奠定基础;基于克里金插值方法建立的岩相概率模型增加岩相模型准确率至94%;以隔层厚度平面分布图为约束条件的确定性建模方法可准确建立砂组及小层间隔层分布模型;在各成因类型夹层井间规模预测的基础上,基于目标的随机模拟方法可以针对不同成因类型夹层的发育形态、数量、规模和趋势分别设定模拟参数,确定性与随机性相结合,实现了辫状河储层精细地质模型的建立。同时,对相关储层的夹层预测具有一定的指导作用。

关键词: 辫状河, 夹层, 成因类型, 井震结合, 夹层预测

Abstract:  Prediction of interlayers in braided river reservoir is a key component in reservoir description. Interlayer predictions have been largely done on the interlayer developmental pattern and channel bar architecture using one single prediction method. Here, based on literature survey, and focusing on the complex interlayers in the braided river reservoir of P filed, South Sudan, we propose an interlayer prediction method on the basis of multiinformation association following genetic analysis of different sand and shale morphologies developed under different depositing conditions. First, in areas where well densities were large, the skeleton profiles and triangular cross sections were established; and scales of different interlayer were confirmed by use of well log and seismic data with high vertical resolution and strong horizontal continuity. Next, based on the lithofacies model, stable barrier model was built by using the deterministic modeling method, constrained by the barrier thickness map. Then, channel and channel bars were simulated in the sand facies by using stochastic method, constrained by sedimentary microfacies. The interlayer model was also established by using stochastic method, constrained by genetic analysis of various types of interlayers. It was established that there were four types of interlayers in the study area, and a fine geological model reflecting their spatial distributions was built on the basis of multiinformation association. Our study found that the scales of interlayers with thickness greater than 2 m can be verified by well and seismic integration. Thus, the scales of interlayers can be quantitatively determined for different layer types and directions, which lays the foundation for predictive model building. Lithofacies probability model based on Kriging interpolation increases lithofacies model accuracy to 94%. The deterministic modeling method, constrained by stable barrier thickness map, can build accurate barrier model for sand layers and sublayers. This objectbased modeling method combines deterministic and stochastic approaches to set parameters such as form, quality, scale and trendfor different interlayers to build a fine geological model of braided river reservoir. Our method may also be applicable for predicting interlayers in other related reservoirs.

Key words: braided river, interlayer, genetic type, well and seismic integration, interlayers prediction

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