石油与天然气地质 ›› 2017, Vol. 38 ›› Issue (1): 121-131.doi: 10.11743/ogg20170113

• 油气地质 • 上一篇    下一篇

北部湾盆地迈陈凹陷区域探井数模分析与油气勘探方向

张伟1,2, 何家雄2, 胡杨3, 刘菊4, 李晓唐2   

  1. 1. 广州海洋地质调查局, 广东 广州 510075;
    2. 中国科学院 广州地球化学研究所 边缘海地质重点实验室, 广东 广州 510640;
    3. 南华大学, 湖南 衡阳 421001;
    4. 中国石油 南方石油勘探有限责任公司, 广东 广州 510290
  • 收稿日期:2015-07-30 修回日期:2016-12-14 出版日期:2017-02-28 发布日期:2017-02-27
  • 通讯作者: 胡杨(1983-),男,博士,油气勘探与地质。E-mail:120583745@qq.com。 E-mail:120583745@qq.com
  • 第一作者简介:张伟(1987-),男,博士,油气与天然气水合物地质。E-mail:zwgmgs@foxmail.com。
  • 基金项目:

    国家自然科学基金项目(41176052);中国科学院战略性先导科技专项(XDA03030301)。

Numerical simulation research on a regional outpost well and its hint on the future hydrocarbon exploration direction of the Maichen Sag, Beibuwan Basin

Zhang Wei1,2, He Jiaxiong2, Hu Yang3, Liu Ju4, Li Xiaotang2   

  1. 1. Guangzhou Marine Geological Survey, Guangzhou, Guangdong 510075, China;
    2. Key Laboratory of Marginal Sea Geology, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou, Guangdong 510640, China;
    3. Nanhua University, Hengyang, Hunan 421001, China;
    4. South Oil Exploration and Development Company, PetroChina, Guangzhou, Guangdong 510290, China
  • Received:2015-07-30 Revised:2016-12-14 Online:2017-02-28 Published:2017-02-27

摘要:

在深入分析北部湾盆地迈陈凹陷西南部边缘Y1井油气地质资料的基础上,采用PetroMod软件开展了该区油气地质及地球化学的数值模拟研究。研究结果表明,该区仅始新统流沙港组二段暗色泥岩达到较好烃源岩有机质丰度标准,但其成熟度较低,尚未达到成熟生烃门限。迈陈凹陷总体上地温场偏低,综合判识确定其成熟生烃门限为埋深2 600 m,比涠西南凹陷及乌石凹陷始新统烃源岩成熟生烃门限明显偏深。由于Y1井未处在生烃凹陷成熟烃源岩有效生烃灶供给范围内,故其不能获得充足的烃源供给,乃至在其局部构造及圈闭中富集成藏,而最终导致Y1井钻探圈闭为无油气聚集的空圈闭。因此,研究区今后应重视寻找古近系烃源岩有效供烃系统之内的有利区带及圈闭目标,以期获得商业性油气勘探的突破。

关键词: 盆地数值模拟, 热演化生烃史, 成熟生烃门限, 烃源供给系统, 迈陈凹陷, 北部湾盆地

Abstract:

Based on the petroleum-geological data of the Y1 well that is located in the southwestern margin of Maichen Sag of the Beibuwan Basin,in this study,the petroleum-geological and geochemical numerical simulation has been conducted using the PetroMod software.The results show that only the dark mudstones in the second section of Eocene Liushagang Group meet the standard of sufficient organic matter abundance to be defined as hydrocarbon source rock,but they have not reached the hydrocarbon generation threshold because of their low maturity.In addition,the geothermal field of the Maichen depression is generally low,and the mature hydrocarbon generation threshold depth,by comprehensive judgment,has been determined as 2 600 m,which is obviously deeper than that of Eocene hydrocarbon source rocks of the Weixinan and Wushi Sags.As Y1 well is out of drainage range of effective hydrocarbon generation,its structure may not have received sufficient hydrocarbon charge,to become a hydrocarbon accumulation in local structures and trap.Thus,this should result in an empty trap where the Y1 well is targeted.Therefore,favorable zones and traps within the effective hydrocarbon drainage zone of Eocene hydrocarbon source rocks should be focused on,in order to achieve a breakthrough of the commercial hydrocarbon exploration.

Key words: numerical simulation of basins, thermal evolution history of hydrocarbon generation, mature hydrocarbon generation threshold, hydrocarbon drainage system, Maichen Sag, Beibuwan Basin

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