新疆石油地质 ›› 2023, Vol. 44 ›› Issue (6): 635-645.doi: 10.7657/XJPG20230601

• 油气勘探 •    下一篇

古龙凹陷姚一段致密油藏成藏主控因素及成藏模式

刘萍()   

  1. 中国石油 大庆油田分公司 采油五厂,黑龙江 大庆 163712
  • 收稿日期:2023-04-06 修回日期:2023-06-15 出版日期:2023-12-01 发布日期:2023-11-29
  • 作者简介:刘萍(1986-),女,湖北襄阳人,工程师,硕士,石油地质,(Tel)0459-4696150(Email)liupingdz@petrochina.com.cn
  • 基金资助:
    国家科技重大专项(2017ZX05071)

Controlling Factors and Models of Hydrocarbon Accumulation in Tight Oil Reservoirs of Yao 1 Member in Gulong Sag

LIU Ping()   

  1. No. 5 Oil Production Plant, Daqing Oilfield Company Limited, PetroChina, Daqing, Heilongjiang 163712, China
  • Received:2023-04-06 Revised:2023-06-15 Online:2023-12-01 Published:2023-11-29

摘要:

综合地震、地质、地球化学、生产测试等资料,在古龙凹陷姚一段致密油藏类型和分布规律研究的基础上,明确其成藏主控因素及成藏模式。结果表明:古龙凹陷姚一段发育5种致密油藏,由古龙向斜向周缘斜坡由砂岩透镜体油藏变为上倾尖灭岩性油藏、断层-岩性油藏和断块油藏,鼻状凸起顶部为断背斜油藏;致密油藏的形成受烃源岩及超压分布、圈闭类型、油源断裂和优质储集层联合控制,青一段湖相泥岩不仅是致密油藏的物质基础,其形成的异常高压是古龙向斜致密油充注的主要动力;大规模成藏前各类圈闭已形成,两侧高部位构造圈闭和构造-岩性圈闭是致密油运移指向区以及有利的聚集部位,主成藏期开启的反转期断层是致密油垂向运移的主要通道,分流河道优质储集层是致密油聚集的有利储集层;各构造单元成藏主控因素和模式存在差异,古龙向斜为“超压驱动、断层垂向输导、局部甜点富集”成藏模式,新站鼻凸为“超压+浮力接力驱动、断层垂向输导、有利圈闭聚集”成藏模式,新肇斜坡为“超压+浮力联合驱替、断-砂接力运移、有利储集层聚集”成藏模式。

关键词: 松辽盆地, 古龙凹陷, 致密油藏, 姚家组, 青山口组, 主控因素, 成藏模式, 分布特征

Abstract:

Based on the seismic, geological, geochemical, and production testing data, the types and distribution patterns of the tight oil reservoirs in the first member of Yaojia formation (Yao 1 member) in the Gulong sag were analyzed, and then the controlling factors and models of hydrocarbon accumulation in these reservoirs were clarified. The results show that five types of tight oil reservoirs are developed in the Yao 1 member such as lenticular sandstone reservoir in the Gulong syncline, updipping pinch-out lithologic reservoir, fault-lithologic reservoir, fault-block reservoir, and fault-anticline reservoir at the top of the nose-like bulge. The formation of tight oil reservoirs is jointly controlled by source rock and overpressure distribution, traps, oil-source faults, and high-quality reservoir beds. The lacustrine mudstones in the first member of Qingshankou formation (Qing 1 member) serve as the material basis for tight oil reservoirs and also create abnormally-high pressure that drove oil charging into the Gulong syncline. Before extensive hydrocarbon accumulation, various traps had been formed, including structural traps and structural-lithological traps at high positions on both sides, which act as the tight oil migration destinations and favorable accumulation sites. The reversal-stage faults that opened during the main oil accumulation phase serve as the primary pathways for vertical oil migration, and high-quality distributary-channel reservoir beds are favorable for tight oil accumulation. The structural units are different in controlling factors and models of hydrocarbon accumulation. In the Gulong syncline, the hydrocarbon accumulation model is “driven by overpressure, vertical migration along faults, and enrichment in local sweet spots”. In the Xinzhan nose-like bulge, the hydrocarbon accumulation model is “first driven by overpressure then by buoyancy, vertical migration along faults, and accumulation in favorable traps”. In the Xinzhao slope, the hydrocarbon accumulation model is “driven by overpressure + buoyancy, fault-sandbody relay-migration, and accumulation in favorable reservoir beds”.

Key words: Songliao basin, Gulong sag, tight oil reservoir, Yaojia formation, Qingshankou formation, controlling factor, hydrocarbon accumulation model, distribution characteristic

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