新疆石油地质 ›› 2005, Vol. 26 ›› Issue (3): 249-252.

• 油气勘探 • 上一篇    下一篇

银根盆地查干凹陷火成岩岩相特征及其识别标志

王惠民1, 靳涛2, 杨红霞2   

  1. 1.中国地质大学北京100083;
    2.中国石油新疆油田分公司勘探开发研究院,克拉玛依 834000
  • 收稿日期:2004-12-29 出版日期:2005-06-01 发布日期:2020-11-23
  • 作者简介:王惠民(1971-),男,新疆玛纳斯人,在读博士研究生,矿产普查与勘探,(Tel)010-82320834(E-mail)wanghuimin2002@sina.com.

Characteristics of Igneous Rock Lithofacies and Its Recognition Marks in Chagan Sag, Yin'gen Basin

WANG Hui-min1, JIN Tao2, YANG Hong-xia2   

  1. 1. China University of Geosciences, Bejing 100083, China;
    2. Research Institute of Exploration and Development, Xinjiang ilfield Company, PetroChina, Karamay, Xinjiang 834000, China
  • Received:2004-12-29 Online:2005-06-01 Published:2020-11-23

摘要: 对银根盆地查 干凹陷中广泛分布着的火成岩相和它们在地震剖面上的识别标志进行了研究,探讨了该区火成岩与油气藏的关系,指出了火成岩油气藏的有利区带。该区火成岩岩相类型有爆发相、溢流相、火山颈相及火山沉积相,尤以溢流相最为发育;依据火山岩类通常以地震波速较高、密度大、磁化率高、电阻率大和地震波吸收能量大的特征,建立了4种火山岩岩相和4种侵入岩岩相的地震识别标志。深大断裂控制着火成岩的分布,同时控制着火成岩圈闭的分布。断裂发育带附近是火成岩油气藏勘探的最有利地区。

关键词: 查干凹陷, 火成岩岩相, 识别标志, 火成岩油气藏

Abstract: The igneous rocks occur widely in Chagan sag of Y in gen basin. This paper presents the study of the igneous rock lithofacies and seismic recognition marks, the discussion of the relations between igneous rocks and oil-gas reservoirs, pointing out the favorable zones of igneous reservoirs. The igneous lithofacies types include explosive facies, overflow facies, volcanic-neck facies and volcano sedimentary facies, of which overflow facies is the most developed. According to the characteristics of the volcanic types such as high seismic wave velocity, high density, high magnetic susceptibility, high resistivity and high absorbability of seismic wave, the seismic recognition marks of four volcanic lithofacies and four intrusive lithofacies are set up. It is concluded that the deep fault controls both distribution of the igneous rocks and distribution of igneous traps. The favorable zones of igneous reservoir prospecting should be near the faul-developed belts.

Key words: Chagan sag, igneous lithofacies, recognition mark, igneous reservoir

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