J4 ›› 2010, Vol. 40 ›› Issue (2): 253-263.

• 地质与资源 • 上一篇    下一篇

松辽盆地幔源成因CO2气藏分布规律及控制因素

付晓飞|沙威|王磊|刘晓波   

  1. 大庆石油学院 |地球科学学院|黑龙江 大庆 163318
  • 收稿日期:2009-05-24 出版日期:2010-03-26 发布日期:2010-03-26
  • 作者简介:付晓飞(1973-)|男|内蒙古赤峰人|副教授|主要从事油气藏形成及资源评价研究|E-mail:fuxiaofei2008@sohu.com
  • 基金资助:

    中国石油天然气股份有限公司重大科技专项(07-02Z-01-01);黑龙江省普通高等学校青年学术骨干支持计划项目(115ZG004)

Distribution Law of Mantle-Origin CO2 Gas Reservoirs and Its Controlling Factors in Songliao Basin

FU Xiao-fei|SHA Wei|WANG Lei|LIU Xiao-bo   

  1. College of Earth Sciences,Daqing Petroleum Institute|Daqing,Heilongjiang 163318|China
  • Received:2009-05-24 Online:2010-03-26 Published:2010-03-26

摘要:

通过深部15s大剖面解译和典型CO2气藏解剖,深入剖析了松辽盆地幔源成因CO2气藏分布规律及控制因素。纵向上CO2气主要富集在营城组火山岩和泉头组三、四段砂岩储层中。与深部热流体(热流底辟体和侵入体)直接相连的、控陷的、控制火山通道的铲式基底断裂控制着CO2气藏呈串珠状分布的特征,断裂走向拐点、端点和侧列叠覆区控制了CO2气出气点。深部热流体是CO2气藏主要的气源。与之相衔接的基底断裂活动导致幔源岩浆充注盆地,同时携带的CO2气释放进入早期喷发的火山岩中形成营城组火山岩CO2气藏。基于控藏断裂多为断陷期和泉头组晚期-青山口组早期活动的基底断裂,推测营城组CO2气藏主要成藏时期为泉头组晚期-青山口组早期。松辽盆地强烈的构造反转发生在明水组末期,挤压应力自南南东向北北西方向衰减的过程中,基底断裂复活形成正反转断层,CO2气从热流底辟体中脱出上运而聚集在反转构造带上,断层式反转构造南部比北部发育,西部比东部发育,因此松辽盆地南部比北部、西部比东部CO2气更富集。

关键词: 松辽盆地, CO2, 气藏, 分布规律, 基底断裂, 热流体, 反转构造

Abstract:

Based on the interpretation of 15s deeper seismic profiles and the anatomy of typical CO2 gas reservoirs, the distribution law of CO2 gas reservoirs and its controlling factors have been deeply analyzed in the Songliao basin. Vertically, CO2 is mainly rich in volcanic rocks of the Yingcheng Formation, and sandstone reservoirs in 3th and 4th Members of Quantou Formation. The beaded distribution feature of CO2 is mainly dominated by lystric basement faults which are in direct contact with deep thermal fluid: heat-flow diapirs and intrusions, and are depression-controlling and volcanic vent-controlling. Meanwhile, outlet points of CO2 are controlled by strike infection-points, endpoints and overlap zones of these faults. And CO2 mainly comes from the deep thermal fluid. The activity of basement faults connected with thermal fluid led to the basin filling by mantle-derived magma, at the same time, the carried CO2 was released into volcanic rocks erupted earlier and then developed into volcanic CO2 gas reservoirs of Yingcheng Formation. Considering that faults controlling gas pool are usually basement faults which were active during fault-depression phase and the Late Quantou Formation to the Early Qingshankou Formation, it was speculated that CO2 reservoirs of Yingcheng Formation were mainly formed between the Late Quantou Formation and the Early Qingshankou Formation. In Songliao basin, the stronge tectonic inversion occurred in the Late Mingshui Formation, and during the declining of compressive force from the SSE to the NNW, the reactivation of basement faults formed positive inversion faults; released from thermal fluid diapirs, CO2  was migrated upward and then accumulated in inversion structural belts; as the development of fault-style inversion tectonics in the southern part is better than the northern part, and the western is better than the eastern part, CO2 is richer in the south than in the north, richer in the west than in the east in Songliao basin.

Key words: Songliao basin, carbon dioxide, gas reservoir, distribution law, basement fault, thermal fluid, inversion tectonics

中图分类号: 

  • P618.13
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