中国石油勘探 ›› 2017, Vol. 22 ›› Issue (2): 50-57.DOI: 10.3969/j.issn.1672-7703.2017.02.006

• 石油地质 • 上一篇    下一篇

西湖凹陷平湖组物源分析

吴嘉鹏1, 张兰2, 万丽芬3, 赵千慧4, 杨彩虹3, 王英民5   

  1. 1. 中国石油集团长城钻探工程有限公司解释研究中心;
    2. 中海石油(中国)有限公司上海分公司;
    3. 中国石化上海海洋油气分公司研究院;
    4. 中国石油天然气管道局国际事业部;
    5. 浙江大学海洋学院
  • 收稿日期:2016-01-04 修回日期:2016-12-14 出版日期:2017-03-10 发布日期:2017-03-10
  • 作者简介:吴嘉鹏(1987-),男,山东新泰人,博士,2014 年毕业于中国石油大学(北京),工程师,现主要从事层序地层、沉积储层综合研究和油气勘探工作。地址:北京市朝阳区安立路 101 号名人大厦,邮政编码:100101。E-mail:wjp_better@sina.com.cn

Provenance analysis of Pinghu Formation in Xihu sag

Wu Jiapeng1, Zhang Lan2, Wan Lifen3, Zhao Qianhui4, Yang Caihong3, Wang Yingmin5   

  1. 1. Geoscience Centre of CNPC Greatwall Drilling Company;
    2. Shanghai Branch of CNOOC Limited;
    3. Research Institute of Sinopec Shanghai Offshore Petroleum Company;
    4. Overseas Business Division of China Petroleum Pipeline Bureau;
    5. Ocean College, Zhejiang University
  • Received:2016-01-04 Revised:2016-12-14 Online:2017-03-10 Published:2017-03-10
  • Contact: 10.3969/j.issn.1672-7703.2017.02.006

摘要: 西湖凹陷平湖组是否存在东侧物源存在争议,东侧物源的确定对油气勘探意义重大。综合利用钻井、地震、分析化验等资料,分析西湖凹陷平湖组沉积物的重矿物ZTR指数、砂岩类型、岩屑组分、砂岩百分含量以及地震相、同沉积构造特征等,发现平湖组沉积物的陆源重矿物ZTR指数及砂岩成分成熟度呈“凹陷两侧低、中间高”的特征,自生重矿物菱铁矿及砂岩百分含量则呈“凹陷两侧高、中间低”分布;由地震反射特征可知,平湖组存在明显的盆地边缘杂乱反射及指示东侧物源存在的前积反射构型;而且平湖组中晚期生长背斜的存在,从构造应力方面进一步印证了平湖组沉积时期东部隆褶带的存在。综合以上研究,认为东部隆褶带在平湖组沉积期就已经隆起并作为西湖凹陷的东侧物源,西湖凹陷中东部深层平湖组具有良好的油气勘探前景。

关键词: 平湖组, 物源分析, ZTR指数, 地震相, 西湖凹陷

Abstract: It is disputable about whether the eastern provenance exists for the Pinghu Formation in the Xihu sag. Its clear answer will be signifcant for hydrocarbon exploration. Based on drilling, seismic, and test data, the Pinghu Formation sediments were analyzed in respect of ZTR index of heavy minerals, sandstone types, debris composition, sandstone content, seismic facies and syndepositional structural features. It is found that the ZTR index of terrigenous heavy minerals and the maturity of sandstone components in the Pinghu Formation are "low at both sides of the sag and high in the middle", while the contents (or percentages) of siderite (an authigenic heavy mineral) and sandstone are "high at both sides of the sag and low in the middle". According to seismic reflection features, the Pinghu Formation has apparent chaotic reflections at basin margin and prograding reflection confguration that indicates the existence of the eastern provenance. Moreover, the existence of growth anticlines during middle-late stage of the Pinghu Formation further proves, from the prospective of tectonic stress, that there was an eastern folded and uplifted belt during the sedimentation of the Pinghu Formation. It is concluded that the eastern folded and uplifted belt had already uplifted and become the eastern provenance during the sedimentation of the Pinghu Formation. The deep Pinghu Formation in central and eastern parts of the Xihu sag has good hydrocarbon exploration prospect.

Key words: ZTR index, seismic facies, Xihu sag, Pinghu Formation, provenance analysis

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