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Formation and evolution of Silurian paleo-oil pools in the Tarim Basin, NW China

机译:塔里木盆地志留系古油藏的形成与演化

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The formation and evolution of Silurian sandstone reservoirs, which are characterized by the coexistence of reservoir bitumen with different types of commercial oil pools in a very extensive area around the slope and uplift areas of the Manjiaer Depression in the Tarim Basin, NW China, are still in question. In this paper we report our investigations on the geological and geochemical characteristics of this reservoir. The results show there are four types of oil shows in the reservoir: severely biodegraded solid bitumen, biodegraded heavy oil, normal oils and light oils with slight biodegradation. Three suites of petroleum inclusions were identified in the reservoir which were formed during the early Devonian Triassic to Cretaceous and late Tertiary. respectively. Petroleum in the Silurian sandstone reservoirs mainly originated from the mid-lower Cambrian source rock and mid-upper Ordovician source rock. The thermal maturity evolution of the source rocks in slope areas has shown that there were three main stages of oil generation that controlled the formation of the above three stages of petroleum inclusions. This evidence indicates that the Silurian reservoir has experienced three petroleum charge events during its geological history. The first charge event occurred during the early Devonian and it resulted in giant paleo-pools, which gradually evolved into the presently widespread bitumen due to the combination of biodegradation and thermal alteration. The second charge covered a long period from Triassic to Cretaceous and probably was related to both the mid-lower Cambrian source rock and the mid-upper Ordovician source rock. The petroleum generated during this stage mixed and interacted with the low matured residual bitumen and eventually formed the present soft bitumen and some residual heavy oils in the reservoirs The third. charge event, mainly associated with the mid-upper Ordovician source rocks occurred, mainly during late Tertiary and accounted for most of the present commercial petroleum pools (mainly normal and light oils). (C) 2008 Elsevier Ltd. All rights reserved.
机译:志留纪砂岩油藏的形成和演化以在中国西北塔里木盆地曼加尔De陷的斜坡和隆起区周围非常广阔的区域内,与不同类型的商业油藏共存为特征。问题。在本文中,我们报告了对该储层的地质和地球化学特征的调查。结果表明,储层中存在四种类型的油:严重生物降解的固体沥青,生物降解的重油,普通油和轻度生物降解的轻油。在储层中确定了三套石油包裹体,它们是在泥盆纪三叠纪早期至白垩纪和第三纪晚期形成的。分别。志留纪砂岩储层中的石油主要来源于中下寒武统烃源岩和中上奥陶统烃源岩。斜坡区烃源岩的热成熟度演化表明,有三个主要的生油阶段控制着上述三个包裹体的形成。该证据表明志留纪储层在其地质历史过程中经历了三次充油事件。第一次装料事件发生在泥盆纪早期,它导致了巨大的古水池,由于生物降解和热蚀变的结合,逐渐演变成目前广泛分布的沥青。第二次装药覆盖了从三叠纪到白垩纪的一段很长时期,可能与中下寒武统烃源岩和中上奥陶纪烃源岩有关。在这一阶段产生的石油与低成熟的残余沥青混合并相互作用,并最终在储层中形成了目前的软沥青和一些残余的重油。装药事件,主要与奥陶纪中上部烃源岩有关,主要发生在第三纪晚期,占目前商业石油储量的大部分(主要是普通油和轻油)。 (C)2008 Elsevier Ltd.保留所有权利。

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