石油学报 ›› 2004, Vol. 25 ›› Issue (6): 23-28.DOI: 10.7623/syxb200406005

• 地质勘探 • 上一篇    下一篇

大巴山前陆盆地形成及演化与油气勘探潜力分析

汪泽成1, 邹才能1, 陶士振1, 李军1, 王世谦2, 赵朝阳3   

  1. 1. 中国石油勘探开发研究院, 北京, 100083;
    2. 西南油气田分公司研究院, 四川成都, 610051;
    3. 华北油田分公司采油四厂, 河北廊坊, 065001
  • 收稿日期:2004-03-12 修回日期:2004-06-14 出版日期:2004-11-25 发布日期:2010-05-21
  • 作者简介:汪泽成,男,1966年10月生,1998年毕业于中国矿业大学,获博士学位,1998~2002年,在中国地质大学和中国石油勘探开发研究院做博士后研究,现为中国石油勘探开发研究院地质所高级工程师,主要从事油气勘探及油气地质研究.E-mail:wangzecheng@petrochina.com
  • 基金资助:
    国家重点基础研究规划项目(2001CB209100)和中国石油天然气股份公司科技攻关项目资助.

Analysis on tectonic evolution and exploration potential in Dabashan foreland basin

WANG Ze-cheng1, ZOU Cai-neng1, TAO Shi-zhen1, LI Jun1, WANG Shi-qian2, ZHAO Chao-yang3   

  1. 1. Research Institute of Petroleum Exploration and Development, Petro China, Beijing 100083, China;
    2. Research Institute of West-South Oil Company, Petro China, Chengdu 610051, China;
    3. The Forth Oil Recovery Plant, Huabei Oil Field Ltd., Langfang 065001, China
  • Received:2004-03-12 Revised:2004-06-14 Online:2004-11-25 Published:2010-05-21

摘要: 根据野外地质调查、地震资料解释以及大量岩心分析化验等资料,探讨了大巴山前陆盆地的形成及演化,分析了油气勘探潜力。研究结果表明,大巴山前陆盆地形成始于燕山中幕,盆地演化经历了J1-J21陆内坳陷湖盆阶段、J22-J3前陆盆地阶段、K1N盆地萎缩阶段以及喜马拉雅期最终定型阶段。大安寨段和凉高山组两套优质烃源岩的有机质丰度高,有机质类型以Ⅱ1型和Ⅱ2型为主。侏罗系发育大安寨段、凉高山组自生自储型和下沙溪庙组下生上储型3套生储盖组合。有利勘探区带包括大巴山前冲断带、川北凹陷带和川中低隆起带。

关键词: 大巴山地区, 前陆盆地, 冲断带, 下沙溪庙组, 河流—三角洲沉积

Abstract: On the basis of outcrop survey,seismic interpretation and a lot of coring data,the evolution and exploration potential of Dabashan foreland basin were analyzed.This foreland basin was formed in the mid-Yanshan cycle and underwent four stages including J1-J21 depression stage,J22-J3 foreland basin stage,K1-N basin shrunk and final deformation of thrust-folded end in Himalayan period.In this basin,two sets of high-quality resource rocks developed in the Daanzhai Formation and Lianggaoshan Formation have high abundance of organic matters which mainly contain Ⅱ1 type and Ⅱ2 type kerogen.The favorable assemblages of source-reservoir-cap rocks in Jurassic include self-generated and self-reservoir type Daanzhai Formation and Lianggaoshan Formation as well as lower-generated and upper-reservoir type lower Shaximiao Formation.The favorable plays include the thrust belt in Dabashan area,sag in the north Sichuan province and uplift in the central Sichuan province.

Key words: Dabashan area, foreland basin, thrust belt, lower Shaximiao Formation, fluvial-delta deposit

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