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首页> 外文期刊>Natural Gas Industry B >Hydrocarbon accumulation of composite-buried hill reservoirs in the western subsag of Bozhong sag, Bohai Bay Basin
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Hydrocarbon accumulation of composite-buried hill reservoirs in the western subsag of Bozhong sag, Bohai Bay Basin

机译:渤海湾盆地博中凹陷西方覆盖山储层的碳氢化合物积累

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摘要

There are abundant hydrocarbon resources in the western subsag of Bozhong sag in the Bohai Bay Basin, where oil–gas discoveries have been made in those shallow Neogene and Paleogene reservoirs and deep Mesozoic buried hill reservoirs, but no better understandings have yet been achieved in terms of the process of hydrocarbon accumulation and the relationship between deep buried hill reservoirs and the allocation of shallow reservoirs. Based on the organic geochemical analysis of source rocks and basin modeling of hydrocarbon generation evolution, distribution characteristics of fluid inclusion and homogeneous temperature measurement, combined with the characteristics of oil-source biomarkers, the process of hydrocarbon accumulation in this study area was resumed based upon the regional tectonic background. The following findings were obtained. (1) There are 3 sets of source rocks in the third and first members of Paleogene Shahejie Fm, and the second lower member of Paleogene Dongying Fm; the reservoirs in the peripheral uplift zones include Mesozoic volcanic rocks, Archean metamorphic rocks, and Paleogene–Neogene delta–fluvial porous sandstones. Hydrocarbon generated in this sag migrated along the fault and the unconformity surface to the slope before accumulated in the peripheral tectonic zones, resulting in 3 sets of source–reservoir–caprock assemblages formed with the characteristics of reservoir formation in compound oil and gas accumulation zones. (2) The stratum in the third member of Shahejie Fm is the main source rock. (3) The above three assemblages went through four periods of generating process during the geological time of 11–1?Ma. Vertically hydrocarbon sources first filled in the deep Mesozoic and Archean reservoirs, then migrated and accumulated in the shallow Neogene and Paleogene reservoirs, where multiple shore-term rapid filling of high-temperature fluids led to this typical oil and gas pooling mode.
机译:渤海湾盆地博中凹陷西部碳水化合物中有丰富的碳氢化合物资源,其中在浅内古和储层和深层中生岩层山区的石油天然气发现,但尚未实现更好的理解碳氢化合物积累的过程及深层埋藏山储层与浅水区分配的关系。基于烃源岩的有机地球化学分析,流体包容性和均匀温度测量的分布特性,结合油源生物标志物的特点,恢复了本研究区内的碳氢化合物积累过程基于区域构造背景。获得了以下发现。 (1)在古雄沙河杰FM的第三个和第一个成员中有3套源岩,以及古古代东营FM的第二个下部成员;外围提升区域中的储存器包括中生代火山岩,阿甲变质岩,古烯 - 新生三角型氟砂岩。在该凹凸中产生的烃沿着故障和非整合表面迁移到斜坡之前在累积在周边构造区域之前,形成3组源储层 - 穴位组合,形成了复合油和气体积聚区中的贮存器形成的特性。 (2)Shahejie FM的第三个成员中的阶层是主要源岩。 (3)上述三个组件经历了在11-1的地质时间期间发电过程的四个时期。垂直烃源首先填充在深层中生代和准储层中,然后在浅内储存器中迁移和累积,其中高温流体的多个梯度快速填充导致该典型的油和气体池。

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