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Role of Seismic Reflection Profiles in Delineating Basin-Centered Geothermal Reservoirs

机译:地震反射剖面在描绘以盆地为中心的地热储层中的作用

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Seismic reflection techniques have not proved very useful in delineating hydrothermal reservoirs in the Great Basin due mainly to the challenging geologic setting of interlayered fan and playa deposits adjacent to steeply down-faulted bedrock. However, basin-centered geothermal reservoirs in the Great Basin offer a much simpler sedimentary setting with sub-horizontal reflectors analogous to most large oil and gas producing basins where seismic reflection imaging is a powerful exploration technique. A review of 1980s-vintage, public-domain COCORP seismic surveys in western Utah and eastern Nevada allows construction of balanced structural cross sections. Important constraints were stratigraphic information derived from numerous nearby oil exploration wells, and outcrop geology exposed in the ranges. Examples are shown for two regions - Black Rock Desert, Utah, and North Steptoe Valley, Nevada - where geothermal reservoirs appear to be located at about 3 km depth. Subsequent evaluation of selected industry seismic reflection data collected over the last 40 years from western Utah and Nevada indicates variable quality, but a potentially valuable data resource for more detailed structural and stratigraphic analysis of basin-centered Paleozoic reservoirs. In some basins there are multiple seismic lines available to be licensed for these studies, making 3D structural modeling of the basins and their associated faults possible at a fraction of the cost of new seismic data acquisition. The Black Rock Desert, Marys River Basin, and North Steptoe Basin are identified as obvious geothermal reservoir targets where industry seismic reflection data will be helpful. A summary map is presented for the Great Basin showing the location of past industry seismic reflection lines and an overlay of major basins derived from gravity surveys. When combined with thermal gradient and heat flow measurements allowing the prediction of the temperature at 3 - 4 km depth, these three geophysical techniques (seismic reflection, gravity, and heat flow) are a powerful tool for prioritizing basin-centered reservoirs most suitable for future power development.
机译:地震反射技术并未证明在大盆地描绘水热储层的主要原因是由于陡峭故障的基岩邻近的夹层风扇和Playa沉积物的挑战性地质凝固。然而,较大的盆地的盆地地热水库提供了更简单的沉积设置,具有类似于大多数大型石油和天然气生产盆地的散水反射器,其中地震反射成像是一种强大的勘探技术。审查犹他州西部和内华达州西部的公共领域的公共领域的传染性,公共领域Cocorp地震调查允许建设平衡结构横截面。重要的制约因素是从众多附近的石油勘探井中获得的地层信息,并在范围内暴露的露头地质。示例显示为两个地区 - 黑色岩石沙漠,犹他州和北斯蒂夫罗谷,内华达州 - 地热水库似乎位于约3公里深度。随后评估在犹他州西部和内华达州过去40年来收集的选定行业地震反射数据表明了可变的质量,而是一种潜在有价值的数据资源,用于盆地古生代水库更详细的结构和地层分析。在一些盆地中,有多种可用的地震线可用于这些研究,使盆地的3D结构建模及其相关的故障在新地震数据采集的成本下可能成为可能的。黑色岩石沙漠,玛丽河流域和北斯蒂芬盆地被确定为明显的地热水库目标,其中行业地震反射数据会有所帮助。提供了一个摘要地图,用于展示过去行业地震反射线的位置和源自重力调查的主要盆地的覆盖层。当与热梯度和热流测量结合时,允许预测3-4公里深度的温度,这三种地球物理技术(地震反射,重力和热流)是优先考虑最适合未来的盆地储层的强大工具电力发展。

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