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Origin of warm springs in Banks Peninsula, New Zealand

机译:新西兰银行半岛温泉的起源

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Thermal springs present rare opportunities to locate and interpret the geological drivers of upper-crustal fluid flow. Interpreting the conditions through which crustal fluids are heated and released to the surface is important for advancing our understanding of crustal deformation and geothermal resource potential across tectonic contexts. In New Zealand, the majority of thermal springs are associated with magmatichydrothermal systems in the central North Island or with the rapidly uplifting bedrock in the South Island's convergent fault systems. However, low enthalpy systems outside of these areas represent attractive targets for potential geothermal resource development. The low enthalpy warm springs of Banks Peninsula, located immediately adjacent to Christchurch, represent a highly understudied but potentially significant resource to the South Island's most densely populated metropolitan area. Hosted within the eroded 11-5.8 Ma volcanic complex of Banks Peninsula, these warm springs (14.5-33.6 degrees C) represent an anomalous hydrothermal system that has been perturbed by the 2010-2016 Canterbury Earthquake Sequence (CES). The February 22, 2011, Mw 6.2 earthquake induced observable changes to the Banks Peninsula warm springs system, including the appearance of new warm springs within the peninsula's north-western Hillsborough Valley. We assess the origins of the volcanically-hosted Banks Peninsula warm springs post-CES using an integrated isotopic, geochemical, and soil gas flux approach. Additionally, we elucidate the tectonic context and geological drivers of upper-crustal fluid flow in the Banks Peninsula warm spring system. Aqueous phase emissions from the springs predominantly plot within the Na+ + K+/HCO3- type waters and exhibit delta O-18, delta D, and delta C-13 values of -8.30 to -9.26% V-SMOW, -60.15 to -64.19 parts per thousand V-SMOW, and -12.37 to -15.06 parts per thousand V-PDB, respectively. Soil gas flux surveys of the springs at Rapaki Bay re
机译:热弹簧提供了罕见的机会,以定位和解释上地壳流体流动的地质司机。解释地壳流体被加热和释放到表面的条件对于推进我们对构造背景的理解,对地壳变形和地热资源潜力的理解是重要的。在新西兰,大多数热弹簧与中央北岛中的Magmatichydrothothothothothotual系统或南岛收敛故障系统中的快速上升基岩相关联。然而,这些区域之外的低焓系统代表了潜在地热资源开发的有吸引力的目标。 Banks Peninsula的低焓温泉,位于基督城,位于基督城邻近,代表了南岛最密集的大都市地区的高度吸引力但潜在的重要资源。这些温泉(14.5-33.6摄氏度)的侵蚀11-5.8 mA火山复合物中托管在侵蚀的11-5.8 mA火山复合物中,代表了由2010-2016坎特伯雷地震序列(CES)扰乱的异常水热系统。 2011年2月22日,MW 6.2地震诱导了银行半岛温泉系统的可观察变化,包括半岛西南山谷山谷内新温泉的外观。我们使用集成同位素,地球化学和土壤气体通量方法评估Volcanipliply的银行半岛温泉温泉的起源。此外,我们阐明了银行半岛温泉系统中的上地壳流体流动的构造背景和地质驱动因素。来自泉水的水相排放主要在Na + + + + / HCO3型水中绘制曲线和表现ΔO-18,Delta D和Delta C-13值-8.30至-9.26%V-Smow,-60.15至-64.19零件每千次V-Smow,分别为-12.37至-15.06份/份每千V-PDB。 Rapaki Bay Re的Springs土壤气体通量调查

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