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Geothermal Exploration at Emerson Pass, Pyramid Paiute Tribal Lands, Nevada

机译:内华达州金字塔派尤特部落土地艾默生erson口的地热勘探

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Five thermal gradient wells were drilled and evaluated as part of a recent collaboration between the Nevada Bureau of Mines and Geology (NBMG) and the Pyramid Lake Paiute Tribe (PLPT) at the Emerson Pass geothermal prospect. Maximum recorded temperatures were 120.8°C at 76 m (250 ft) in one of the wells drilled by the PLPT. A subsequent deeper well drilled by NBMG to 305 m (1000 ft) showed a maximum temperature of 117°C at 168 m (550 ft), with temperatures decreasing below that depth indicating a broad outflow zone between approximately 79 to 238 m (260 to 780 ft) below ground surface at ~115°C. Existing data indicate that the shallow, maximum temperature zone of ≈120°C may be of fairly limited spatial extent based on the size of a vegetation dead zone and the near surface expression of an anomalous temperature zone depicted by several shallow temperature surveys. A deeper higher temperature reservoir could be present, although its temperature and extent remain unconstrained.
机译:内华达州矿业与地质局(NBMG)与艾默生山口地热勘探区的金字塔派尤特部落(PLPT)最近的合作中,钻了五口热梯度井并进行了评估。在PLPT钻的其中一口井中,最高记录温度是76 m(250 ft)处的120.8°C。随后由NBMG钻至305 m(1000 ft)的更深井显示最高温度为168 m(550 ft)时为117°C,温度下降到该深度以下表示大约79至238 m(260至250 m)之间的宽流出区域。在约115°C下低于地面780英尺)。现有数据表明,基于植被死区的大小和几次浅层温度调查所描绘的异常温度带的近地表表达,≈120°C的浅层,最高温度带的空间范围可能相当有限。尽管温度和范围不受限制,但仍可能存在更深的高温储层。

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