渤海湾盆地黄骅坳陷深层煤系油气成藏机理与模式

Runze Yang , Haitao Liu , Hongjun Li , Changyi Zhao , Chuanming Li
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引用次数: 2

摘要

煤系地层油气成藏分为源内成藏和调整成藏两种类型,特别是在经历了多期构造活动的盆地中。控制这种积累的机制极其复杂。以黄骅坳陷古生界含油气系统为例,通过岩心观察、煤系烃源岩地球化学测试、薄片观察、流体包裹体测试和典型储层剖面分析,结合地层埋藏史和热史,揭示了深层油气成藏机理。从区域构造出发,明确了煤系油气成藏机理,建立了煤系油气成藏模式。结果表明,黄骅坳陷古生界含油气系统存在源下、源内、源上三种不同类型的生储盖组合。区域构造演化控制着烃源岩的生烃过程,呈现出“早期油,后期气”的生烃特征。中白垩世是两期油气成藏的第一期,这一阶段以低成熟油为主,少量天然气主要储存在粒间孔隙和溶蚀孔隙中。晚白垩世构造隆升导致古储层的破坏。第二次成藏期发生在中古近纪至今。大量天然气和高成熟度原油主要富集在溶蚀孔隙和构造裂缝中。黄骅坳陷油气成藏受储层改造、构造活动和烃源岩成熟共同调控。在上述认识的基础上,提出了煤系“油气中转站”成藏模式,即油气先在源内或近源储层聚集,然后在构造活动的作用下由“油气中转站”向其他区域转移。
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Accumulation mechanism and model of coal measure derived oil and gas in the deep reservoir of Huanghua Depression, Bohai Bay Basin, China

Hydrocarbon accumulation in coal measure strata is consist of several types which includes intra-source accumulation and adjusted accumulation, particularly in basins that had experienced multi-stage tectonic activities. The mechanism governing this accumulation is extremely complex. Using the Paleozoic petroleum system in the Huanghua Depression as an example, the mechanism of hydrocarbon accumulation in deep reservoirs can be revealed by means of core observation, geochemistry testing of coal measure source rock, thin section observation, fluid inclusions testing, and profile analysis of typical reservoirs, combined with the burial and thermal history of strata. Based on the regional tectonic, the mechanism of hydrocarbon accumulation in coal measures is defined and the accumulation model was established. The results show that the Paleozoic petroleum system in the Huanghua Depression has three different types of source-reservoir-cap assemblages: under-source, intra-source, and above-source assemblage. Regional tectonic evolution controlled the hydrocarbon generation process of source rocks, showing the hydrocarbon generation characteristics of “oil in the early stage and gas in the late stage.” The Middle Cretaceous is the first of two periods of hydrocarbon accumulation, during which stage occurred in low-maturity oil and a small amount of natural gas were mainly stored in intergranular pores and dissolution pores. The tectonic uplift in the Late Cretaceous caused the destruction of the ancient reservoir. The second accumulation stage occurred in the Middle Paleogene to the present. A large amount of natural gas and high maturity oil were mostly stored in dissolution pores and structural fractures. The hydrocarbon accumulation in Huanghua Depression was simultaneously regulated by reservoir reformation, tectonic activities, and source rock maturation. Based on the foregoing understanding, the hydrocarbon accumulation model of “oil and gas transfer station” in coal measures is put forward, that is, oil and gas are first accumulated in intra-source or near-source reservoirs, and are then adjusted from this “oil and gas transfer station” to other areas as a result of tectonic activity.

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