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首页> 外文期刊>Energy Exploration & Exploitation >Hydrocarbon accumulation and formation of composite reservoirs in KLI6-I of Laizhou Bay Sag, Bohai Sea, China
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Hydrocarbon accumulation and formation of composite reservoirs in KLI6-I of Laizhou Bay Sag, Bohai Sea, China

机译:渤海莱州湾凹陷KLI6-I复合油气藏成藏

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摘要

The Laizhou Bay Sag, one of the oil-bearing sags with large exploration potential in the South Bohai Sea of China, contains two sets of high-quality hydrocarbon source rocks, i.e. Member 3 and Member 4 of Shahejie Fm (E(2)s(3) and E(2)s(4)). As an important hydrocarbon accumulation zone in the sag, the KL16-1 low bulge is found to have oil reservoirs in the Neogene Guantao Fm (N(1)g), the Paleogene Dongying Fm (E(3)d), the Paleogene Shahejie Fm (E(2)s), and the Mesozoic buried hill formation. It is characterized by distinct features of composite reservoirs. Nonetheless, its hydrocarbon accumulation process and mechanism are unknown yet. In this paper, the hydrocarbon generation modelling of source rocks, combined with the characteristics of oil-source rock biomarker compounds and fluid inclusions, is used to restore the hydrocarbon accumulation process in the KL16-1 low bulge. Crude oil in all three KL16-1 plays is characterized by low Pr/Ph, low gammacerane, high 4-methyl sterane and high dinosterane. In other words, it is oil of low maturity to maturity. As the biomarker index of the oil is very similar to that of the E(2)s(3) source rocks, it is thought that E(2)s(3) is the primary source rock layer, while E(2)s(4) is the secondary source rock layer. In addition, episodic oil and gas charging happened in two phases under high pressure in the late period (from 5.0 Ma till now).
机译:莱州湾凹陷是中国渤海南部具有较大勘探潜力的含油凹陷之一,包含两组优质烃源岩,即沙河街组三段和四段(E(2)s (3)和E(2)s(4))。作为凹陷的重要油气聚集区,KL16-1低凸起在新近系陶陶组(N(1)g),古近东营组(E(3)d),古近系沙河街发现有油藏。 Fm(E(2)s)和中生代潜山构造。它具有复合储层的独特特征。但是,其油气成藏过程和机理尚不清楚。本文利用烃源岩生烃模型,结合油源岩生物标志物和流体包裹体的特征,恢复了KL16-1低凸起的油气成藏过程。在这三个KL16-1油田中,原油的特征是低Pr / Ph,低γ-甘油,高4-甲基甾烷和高癸甾烷。换句话说,它是成熟度低至成熟的油。由于石油的生物标志物指数与E(2)s(3)烃源岩的生物标志物指数非常相似,因此认为E(2)s(3)是主要烃源岩层,而E(2)s (4)是次生烃源岩层。此外,在晚期(从5.0 Ma到现在),高压下的间歇性油气充注发生在两个阶段。

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