石油与天然气地质 ›› 2003, Vol. 24 ›› Issue (1): 12-17.doi: 10.11743/ogg20030103

• 油气空间 • 上一篇    下一篇

松辽盆地中生代火山岩油气藏特征

宋维海1, 王璞珺1, 张兴洲1, 蒙启安2, 单玄龙1, 程日辉1   

  1. 1. 吉林大学地球科学学院, 吉林长春, 130061;
    2. 大庆油田有限责任公司勘探开发研究院, 黑龙江大庆, 163712
  • 收稿日期:2002-04-16 出版日期:2003-03-25 发布日期:2012-01-16
  • 基金资助:

    国家自然科学基金资助课题(NSFC)49894190-12

CHARACTERISTICS OF MESOZOIC VOLCANIC RESERVOIRS IN SONGLIAO BASIN

Song Weihai1, Wang Pujun1, Zhang Xingzhou1, Meng Qi'an2, Shan Xuanlong1, Cheng Rihui 1   

  1. 1. College of Earth Sciences, Jilin University, Changchun, Jilin;
    2. Daqing Exploration & Development Institute, Daqing, Heilongjiang
  • Received:2002-04-16 Online:2003-03-25 Published:2012-01-16

PDF (PC)

552

被引次数

129

摘要：

松辽盆地中生代火山岩油气藏主要形成于晚侏罗—早白垩世火山-沉积序列中。在火山-断陷成盆期,深湖相泥质岩与火山岩呈现垂向或侧向的接触关系,是火山岩油气藏形成的主要因素。火山岩储层岩石类型主要包括熔岩类、火山碎屑岩类。火山岩储层主要发育在溢流相,尤其是溢流相顶底部的气孔带是最为有利的储集相带。火山岩储集空间可分为原生孔隙、次生孔隙和裂缝3种类型。区内火山岩油气藏主要受NNE向和近EW向两组区域大断裂控制,大多分布在区域性断裂活动带、基底隆起或构造带上。

关键词: 火山岩, 油气藏, 二元结构, 区域断裂, 松辽盆地

Abstract:

The Mesozoic volcanic reservoirs in Songliao basin formed in the Late Jurassic to Early Cretaceous volcanic-sedimentary sequences. The vertical or lateral contacts between the deep lacustrine argillaceous rocks and volcanic rocks are the key factors of the formation of volcanic reservoirs during the volcanic-fault depression period—basin forming. Rock types of volcanic reservoirs include mainly lava and pyroclastic rock.The major volcanic reservoirs are mainly in the effusive facies, and the best reservoir belts are in the gas cavity belts on top and at base of the effusive facies. The reservoir spaces can be divided into primary pores, secondary pores and fissures. The volcanic reservoirs are mainly controlled by both NNE and nearly EW regional faults, most of them occur in active regional fault zones, basement uplifts or tectonic zones.

Key words: volcanic rocks, hydrocarbon reservoirs, two-component structure, regional fault, Songliao basin

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