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

机译:地震反射曲线在划塑盆地地热储层中的作用

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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:地震反射技术在划定了巨大的盆地中的水热储层,主要是由于靠近陡峭故障的基岩靠近的夹层的地质设置挑战了较大的盆地的热水储层。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的盆地,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和东部东部的公共领域的葡萄酒,公共领域的传播者抗震抗震措施允许建设平衡结构横截面。重要的制约因素是来自众多附近的石油勘探井的地层信息,并且在范围内暴露的露头地质。示例显示了两个地区 - 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公里深处。随后评估在犹他州西部和内华达州的过去40年内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,用于盆地中心古生代水库更详细的结构和地层分析。在一些盆地中,有多种可用于这些研究的许多地震线,使盆地的3D结构建模及其相关的故障在新的地震数据采集的成本中可能成为可能的。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库目标,其中行业地震反射数据将有所帮助。提供了一个汇总图,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)是一个强大的工具,用于优先考虑最适合未来的盆地居中的储层电力发展。

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