新疆石油地质 ›› 2005, Vol. 26 ›› Issue (5): 481-484.

• 油气勘探 • 上一篇    下一篇

准噶尔盆地非构造油气藏成因类型及成藏主控因素

杨文孝   

  1. 中国石油 新疆油田分公司 勘探开发研究院, 新疆 克拉玛依 834000
  • 收稿日期:2005-04-22 出版日期:2005-10-01 发布日期:2020-11-23
  • 作者简介:杨文孝(1935-),男,四川双流人,教授级高工程师,石油地质,(Tel)0990-6881846

Main Factors of Petroleum Accumulations and Origin Types of Non-Structural Reservoirs in Junggar Basin

YANG Wen-xiao   

  1. Main Factors of Petroleum Accumulations and Origin Types of Non-Structural Reservoirs in Junggar BasinYANG Wen-xiao(Research Institute of Exploration and Development, Xinjiang 0Oilfield Company, PetroChina, Karamay, Xinjiang 834000, China
  • Received:2005-04-22 Online:2005-10-01 Published:2020-11-23

摘要: 准噶尔盆地非构造油气藏发现早、类型多、规模大、分布广、差异大,占已探明石油地质储量的76.1%,一直是新疆石油勘探开发的主要对象。已发现的非构造油气藏储集体成因类型主要包括4类:一是西北缘同生断阶陡坡带洪积扇砾岩、砂砾岩为储集层的断层-岩性及岩性-地层油气藏;二是准东断坡近岸三角洲水下扇、浊积扇砂砾岩、砂岩为储集层的构造-岩性及岩性-地层油气藏;三是腹部古凸起控制的侏罗系-白垩系缓坡带河流-三角洲砂岩为储集层的构造-岩性及岩性-地层油气藏;四是海西运动期基底潜山风化壳油气藏。它们以上三叠统白碱滩组(黄山街组)盆地级区域盖层为界,划分为上、下两大成藏组合。下组合油气来源为自源、近源,其非构造油气藏形成主要是储集体岩相、物性、输导体系3因素控制;上组合油气来源主要为二叠系远源及二叠系和侏罗系烃源的混源,其非构造油气藏的形成,主要受输导体系、构造背景、储集体岩相、圈闭及物性5因素控制。

关键词: 准噶尔盆地, 非构造油气藏, 储集体成因类型, 主控因素

Abstract: Junggar basin is characterized by early discovery, multiple types, large scale, wide distribution and big differences of oil-gas reservoirs, accounting for 76.1% of proved 00IP. It has been playing a major target for petroleum exploration and development in Xinjiang region. For discovered non-structural reservoirs, their onigin types mainly inelude: the fractured-lithologic and lithologic stratigraphic reservoirs dominated by torrential fanglomerale and glutenite of steep slope in depositional fault bench in northwestem margin of Junggar basin, the structural-lithologic and lithologic-stratigraphic reservoirs by delta submarine fan, turbidite fan glutenite and sandstone in nearshore fault slope in Zhundong (east Junggar) area, the structural-lithologic and lithologic stratigraphic reservoirs by fluvial-delta sand-stone in Jurassic-Cretaceous gentle slope controlled by paleo-swell in hinterdand of Junggar basin, and the buried-hill-weathered-crust reservoirs of Hercynian episode in basement of Junggar basin. The basin-scale regional cap rocks of Baijiantan formation (Huangshanjie formation) of Upper Triassic are their boundaries, and upper and lower reservoir assemblages can be divided. The lower assemblage con-tains hydrocarbon from self source and adjacent source, and its main factors of fomming non-structural reservoir are lithofacies, petrophysi-cal property and transport system. The upper assemblage has hydrocarbon sources mainly from Permian remote source and Permian-Jurassic mixed source, its primary control factors of shaping non-structural reservoir are transport 8ystem, tectonic setting, lithofacies, trap and petrophysical property.

Key words: Junggar basin, non-structure, reservoir, origin type, master control factor

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