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潜山储层定量预测技术研究与应用

陈人杰 刘杰 徐乐意 刘徐敏 胡坤

石油物探2024,Vol.63Issue(1):229-237,9.
石油物探2024,Vol.63Issue(1):229-237,9.DOI:10.12431/issn.1000-1441.2024.63.01.020

潜山储层定量预测技术研究与应用

Quantitative characterization of buried-hill reservoirs:A case study of a buried hill in Huizhou sag,Pearl River Mouth Basin

陈人杰 1刘杰 1徐乐意 1刘徐敏 1胡坤1

作者信息

  • 1. 中海石油(中国)有限公司深圳分公司,广东深圳 518000
  • 折叠

摘要

Abstract

The ancient buried hills formed by complicated tectonic movements in the Huizhou sag,the Pearl River Mouth Basin fea-ture large buried depth and strong reservoir heterogeneity.After forty years of exploration and development,it becomes increasing-ly challenging to characterize sweet-spot reservoirs and complicated fractures inside buried hills.Based on the genetic mechanism of buried-hill reservoirs,we investigate major controls on reservoirs in weathered fracture zones and internal fracture zones and estab-lish key techniques for quantitative prediction of buried-hill reservoirs.For weathered fracture zones,we derive a new elastic param-eter from the Keys-Xu model to improve sweet-spot identification and use prestack elastic inversion to predict sweet-spot reser-voirs.For internal fracture zones,we use ant tracking to estimate dominant azimuths of fractures and then integrate equally weigh-ted azimuthal data for fracture prediction.These techniques have offered effective support to the exploration and evaluation of a buried hill,H,in the Huizhou sag and may be applied to buried-hill exploration in additional prospects in the Pearl River Mouth Basin.

关键词

珠江口盆地/潜山/储层预测/风化裂缝带/内幕裂缝带

Key words

Pearl River Mouth Basin/buried hill/reservoir prediction/weathered fracture zone/internal fracture zone

分类

天文与地球科学

引用本文复制引用

陈人杰,刘杰,徐乐意,刘徐敏,胡坤..潜山储层定量预测技术研究与应用[J].石油物探,2024,63(1):229-237,9.

基金项目

中国海油集团公司"十四五"重大科技项目(KJGG2022-0403)资助.This research is financially supported by the Major Science and Technology Projects of China National Offshore Oil Corporation during the 14th Five Year Plan(Grant No.KJGG2022-0403). (KJGG2022-0403)

石油物探

OA北大核心CSTPCD

1000-1441

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