首页> 外文会议>Geothermal Resources Council Annual Meeting >Geothermal Potential of the Pyramid Lake Paiute Reservation, Nevada, USA: Evidence of Previously Unrecognized Moderate-Temperature (150-70 deg C) Geothermal Systems
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Geothermal Potential of the Pyramid Lake Paiute Reservation, Nevada, USA: Evidence of Previously Unrecognized Moderate-Temperature (150-70 deg C) Geothermal Systems

机译:美国内华达州金字塔湖邮政预留的地热潜力:以前未被识别的中等温度(150-70℃)地热系统的证据

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At least two and possibly three previously unrecognizedmoderate-temperature (150-165 deg C) geothermal areas have been identified during a geothermal exploration program on the Pyramid Lake Paiute Reservation (PLPR) in west-central Nevada, USA. At each of these new areas --Pyramid Rock, the southwestern Smoke Creek Desert (SWSMD), and east Astor Pass, -- as well as at the known Needle Rocks geothermal area, hot springs and/or near-surface upwellings of hot water are associated with calcium carbonate (tufa) towers forming today in Pyramid Lake or formed in late Pleistocene Lake Lahontan. The structural controls on geothermal fluid flow are still being investigated, but the intersection of Quaternary faults appears to have localized the shallow upwelling of thermal fluids. Near-surface thermal waters, where identified, have temperatures ranging up to 49-97 deg C, whereas quartz and Na-K-Ca-Mg geothermometers suggest reservoir temperatures on the order of approx150 to 165 deg C. Exploration work began with compilation of existing data into a geothermal geographic information system (GIS), and acquisition of an airborne hyperspectral remote-sensing survey of the entire reservation. These efforts were followed by a reconnaissance field survey that prioritized the investigation of anomalies identified in the initial GIS and hyperspectral work. The field survey, which included temperature measurements of springs and existing wells; reconnaissance structural and geological assessments; and geochemical analyses of selected spring and well waters, identified the current areas of interest. Two promising areas have been investigated in detail with magnetic and gravity surveys; shallow temperature measurements from 2-meter-deep auger holes; detailed geologic mapping; and temperature-gradient drilling. Temperature-gradient drilling is in progress, and early results include the intersection of near-boiling waters within 60 m (200 ft) of the surface just east of Astor Pass, approx6 km northwest of Needle Rocks in an area with no springs.
机译:在美国西部内华达州西部 - 中部的金字塔湖Paiute预订(PLPR)的地热勘探计划中,至少有两个和可能三个先前未被识别的过热剂(150-165℃)地热区域。在这些新的领域 - 罗拉米德岩石,西南烟溪沙漠(SWSMD)和东斯特罗斯通行证, - 以及已知的针头岩石地热区域,温泉和/或近地表面升空的热水与今天在金字塔湖中形成的碳酸钙(Tufa)塔有关,或在Lahontan Lahontan湖后期形成。仍在研究地热流体流动的结构控制,但季外断层的交叉似乎是热流体的浅层升高。近视的近表面热水,在鉴定,温度范围内高达49-97℃,而石英和Na-K-CA-Mg地热测定仪建议储层温度约为150至165℃。勘探工作开始于汇编现有数据进入地热地理信息系统(GIS),并获取整个预留的空中高光谱遥感调查。这些努力其次是优先在初始GIS和高光谱工作中发现的异常现象的调查侦察实地调查。该田间调查包括弹簧和现有井的温度测量;侦察结构和地质评估;和选定的弹簧和井水的地球化学分析,确定了当前的感兴趣区域。用磁性和重力调查详细研究了两个有希望的地区; 2米深螺旋孔的浅温度测量;详细的地质映射;和温度梯度钻孔。温度梯度钻探正在进行中,早期结果包括近60米(200英尺)内的近沸水在Astor Pass的东部,在没有弹簧的一个区域的针岩的大约6公里。

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