中国中西部前陆冲断带盖层品质与油气成藏
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本文为中石油中青年创新基金项目(编号 06E1007)、黑龙江省普通高等学校青年学术骨干支持计划项目和大庆石油学院研究生基金(编号 dky001)的成果。


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Caprock Quality and Hydrocarbon Accumulation in the Basins of Foreland Thrust Belts, Central and Western China

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    摘要:

    中西部前陆盆地沉积演化经历前前陆盆地克拉通沉积、早期前陆盆地沉积、中生代坳陷盆地沉积和新生代再生前陆盆地沉积四个阶段,共发育四种类型的盖层:即克拉通或海陆过渡期盖层、湖沼相煤系盖层、氧化宽浅湖或边缘海相膏泥岩盖层和湖相泥岩盖层。通过叠合型(准噶尔南部(准南))、改造型(川西)和新生型(柴达木北缘(柴北缘))三种典型的前陆盆地各套盖层岩性、盖层岩石累积厚度、盖层岩石占地层厚度的比值、盖层岩石单层厚度、岩石力学特征和盖层封闭烃柱高度定量对比分析,认为川西盖层封闭能力总体优于准南,准南各套盖层封闭能力又优于柴北缘,柴北缘上新统上下油砂山组盖层品质较差,准南中新统塔西河组、柴北缘渐新统上干柴沟组和始新统路乐河组盖层品质较好,其余盖层品质为好。品质好的盖层分布于储盖组合Ⅱ(晚三叠世—侏罗世前陆盆地或坳陷盆地陆相沉积阶段形成的储盖组合)和Ⅲ(晚侏罗世—古近纪陆内坳陷磨拉石沉积阶段形成的储盖组合)中,组合Ⅱ中为中生代湖沼相煤系盖层,控制着自生自储原生油气藏的聚集和保存,组合Ⅲ中多为古近系氧化宽浅湖或边缘海相膏泥岩盖层,对断层沟通下伏烃源岩或调整早期油气到组合Ⅲ中聚集成藏起到重要的封盖作用。受品质好盖层控制,中西部前陆盆地油气主要富集在储盖组合Ⅱ和Ⅲ中。

    Abstract:

    The basins of foreland thrust belts in the central and western China has experienced four stages of deposition evolution,namely craton deposition, early foreland deposition, Mesozoic depression basin deposition and Cenozoic regeneration foreland basin deposition. There have developed four types of caprock, namely Kraton or transitional facies caprock, limnetic facies coal measure caprock, oxidation basin valley or adjacent marine facies cream mudstone caprock,and lacustrine mudstone caprock. Quantitative and comparative analysis of caprock lithology, accumulation thickness, thickness ratio of caprock to total strata, thickness of individual layer, lithomechanics characteristics and hydrocarbon column sealed by caprock of three types of foreland basin, i.e. folding (southern Jungar basin), alternation (western Sichuan basin) and anagenesis (northern margin of the Qaidam basin), indicates that the sealing ability of western Sichuan basin is better than that of southern Jungar basin, the sealing ability of southern Jungar basin is better than that of northern margin of the Qaidam basin, the quality of caprock of Youshashan group up and down of northern margin of the Qaidam basin Pliocene is bad, the sealing ability of Taxihe group of southern Jungar basin Miocene , Shangancaigou of Oligocene and Lulehe group Eocenef northern margin of the Qaidam basin is good, and the rest are best. The caprocks with the best quality are located in the association of reservoir and caprock of Ⅱ (T3 —J association of foreland basin or continental depression basin) and Ⅲ (J3 —P Molass e association of intracontinental depression). The associationⅡ is Mesozoic coal measure caprock of limnetic facies, which controls the accumulation and reservation of self-generation and self-reservation of original hydrocarbon reservoir; the association Ⅲ is Tertiary mudstone caprock of oxidation basin valley or adjacent marine facies cream, which plays an important part in sealing the oil and gas that is linked to hydrocarbon source rock underlying the faults, or is adjusted to the association Ⅲ. Controlled by best quality caprock, the oil and gas mainly concentrate in the association of reservoir and caprock ofⅡand Ⅲ in the foreland basin of the central and western China.

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付晓飞,刘小波,宋岩,柳少波.2008.中国中西部前陆冲断带盖层品质与油气成藏[J].地质论评,54(1):82-93,[DOI].
.2008.[J]. Geological Review,54(1):82-93.

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  • 收稿日期:2007-07-22
  • 最后修改日期:2007-10-16
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