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首页> 外文期刊>Petroleum Geoscience >Controls on reservoir compartmentalization of an Upper Permian tight gas field in Germany and links to a modern analogue in the Western US
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Controls on reservoir compartmentalization of an Upper Permian tight gas field in Germany and links to a modern analogue in the Western US

机译:控制德国上二叠纪致密气田的储层划分,并与美国西部的现代类似物联系起来

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This study focuses on the reservoir characteristics of a Permian tight gas field in the Southern Permian Basin, Eastern Frisia, Germany. To improve the understanding of the reservoir, 3D seismic, wireline and core data were compared with a reservoir analogue in the Panamint Valley, United States. Depositional environments of the Permian Upper Rotliegend II include perermial saline lakes, coastal parallel sand belts comprising wet, damp and dry sand flats and aeolian dunes with interdune deposits. Polygonal patterns at different scales were observed on seismic horizon slices in the reservoir intervals and the overlying Zechstein. Outlines of superordinate polygons coincide with interpreted faults. Similar polygonal networks were identified on modem dry lakes in the western United States. The kilometre-long, up to 1.20 m deep open fissures in the Panamint Valley are interpreted to originate from the combined effects of synaeresis and tectonics. Subsequently, the fissures were filled with aeolian sediment. Vegetation growth confined to the lineaments indicates enhanced fluid circulation. Such fissures systems may serve as weakness zones and fault grain and impact reservoir quality in terms of hydraulic connectivity of reservoir compartments. For the Rotliegend reservoirs, original porosities and permeabilities of these zones were reduced to a minimum by enhanced cementation along the fluid migration pathways. Permeability barriers and reservoir compartmentalization, which can be clearly depicted on seismic attribute volumes, are a potential result of this development.
机译:这项研究的重点是德国东部弗里西亚南部二叠纪盆地二叠系致密气田的储层特征。为了提高对储层的了解,将3D地震,电缆和岩心数据与美国Panamint山谷中的储层类似物进行了比较。二叠纪上罗特里根德二世的沉积环境包括蠕虫盐湖,由湿,湿,干沙滩组成的沿海平行砂带和带有沙丘沉积物的风沙丘。在储层层段和上覆的Zechstein地震视层上观察到了不同比例的多边形图案。上级多边形的轮廓与解释的断层重合。在美国西部的现代干旱湖上也发现了类似的多边形网络。 Panamint山谷中长达一千米,深达1.20 m的开放裂缝被解释为源于结岩作用和构造学的共同作用。随后,裂缝中充满了风沙。局限在植被中的植被生长表明流体循环增强。就储层隔室的水力连通性而言,此类裂缝系统可作为薄弱带和断层颗粒,影响储层质量。对于Rotliegend储层,通过沿流体运移路径增强胶结作用,将这些区域的原始孔隙度和渗透率降至最低。渗透性障碍和储层分隔,可以在地震属性卷上清楚地描绘出来,是这种发展的潜在结果。

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