西南石油大学学报(自然科学版) ›› 2020, Vol. 42 ›› Issue (1): 69-77.DOI: 10.11885/j.issn.1674-5086.2018.09.10.03

• 地质勘探 • 上一篇    下一篇

伊拉克A油田地震异常体识别与成因分析

刘俊海, 徐明华, 王自明, 韩翀, 王海峰   

  1. 中国石油天然气集团有限公司川庆钻探工程有限公司地质勘探开发研究院, 四川 成都 610051
  • 收稿日期:2018-09-10 出版日期:2020-02-10 发布日期:2020-02-10
  • 通讯作者: 刘俊海,E-mail:liujh_dyy@cnpc.com.cn
  • 作者简介:刘俊海,1976年生,男,汉族,河南鹤壁人,工程师,博士,主要从事地震资料解释和石油地质综合研究工作。E-mail:liujh_dyy@cnpc.com.cn;徐明华,1973年生,男,汉族,重庆万州人,高级工程师,博士,主要从事地震资料处理、解释及储层预测方面的研究工作。E-mail:xumh_sc@cnpc.com.cn;王自明,1973年生,男,汉族,四川渠县人,副研究员,博士,主要从事油气藏综合评价、油气田开发方面的研究工作。E-mail:wangzm_dyy@cnpc.com.cn;韩翀,1981年生,男,汉族,河南南阳人,工程师,博士,主要从事油气储层预测研究工作。E-mail:hanchong_dyy@cnpc.com.cn;王海峰,1977年生,男,汉族,河南南阳人,高级工程师,博士,主要从事油气田开发地质综合研究工作。E-mail:642925181@qq.com
  • 基金资助:
    中国石油天然气股份有限公司重大科技专项(2011E-2501)

Seismic Reflection Anomaly Identification and Origin Analysis of A Oilfield in Iraq

LIU Junhai, XU Minghua, WANG Ziming, HAN Cong, WANG Haifeng   

  1. Geological Exploration and Development Research Institute of Chuanqing Drilling Engineering Co. Ltd., CNPC, Chengdu, Sichuan 610051, China
  • Received:2018-09-10 Online:2020-02-10 Published:2020-02-10

摘要: A油田地震资料上广泛存在地震反射异常,其表现为地震同相轴局部的下凹、错断,目前对地震异常体识别及成因机制未开展深入研究,没有取得明确的认识,影响了研究区油气勘探进程。利用相干、方差、似然等多种地震属性进行了地震异常体识别。结果表明,地震异常体横向延伸距离很短,纵向延伸距离变化较大,从几十米到上千米不等,其在平面上为近似圆形,多数没有明显的分布规律,少数为线状或雁列状分布。根据目的层构造演化过程、地应力及岩芯资料对地震异常体成因进行了综合分析。结果表明,地震反射异常体是溶蚀作用和挤压作用的综合结果。早期目的层发生了溶蚀作用,但溶蚀作用强度在平面上和垂向上分布不均匀,由于后期挤压作用较弱,只在局部脆弱的地方发生了断裂。部分异常体是目的层主要纵向油气运移通道,破坏了下部层系圈闭的完整性。

关键词: 碳酸盐岩, 地震反射异常体, 成因分析, 溶蚀作用, 挤压作用

Abstract: In Oilfield A there are many seismic reflection anomalies which is concave or broken seismic event. At present, there is a lack of in-depth research and clear understanding of identification and origin of seismic anomalies, which has affected the oil and gas exploration process. Coherence, variance and likelihood seismic attributes are used to identify seismic reflection anomaly. The results indicate seismic anomaly extends shortly laterally but extends from dozens of meters to a kilometer vertically, and they are of subcircular shape in plan view, most of which are irregular distribution and few of which is linear or echelon distribution. A comprehensive analysis of the origin of seismic anomaly is made based on structural evolution, stress and core data of target formation. The results indicate that seismic reflection anomalies are the combined result of dissolution and compression. Dissolution develops in target formation but development intensity is uneven horizontally and vertically. Because late compression is weak, fault is generated in fragile area of target formation. Some seismic anomalies are the vertical path of oil migration and some seismic anomalies destroy trap of lower formation.

Key words: carbonate rock, seismic reflection anomaly, origin analysis, dissolution, compression

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