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3D Geological modelling of the Taupo Volcanic Zone as a foundation for a geothermal reservoir model

机译:陶波火山带的3D地质建模作为地热储层模型的基础

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We present a 3D hydrogeological model of the central Taupo Volcanic Zone (TVZ), including seven geothermal fields. A combination of borehole data, surface geology and structures were used to generate representative geological groups at depth. The geological units in the model area have been combined into seven hydrogeological groups based primarily on rock types with similar hydraulic characteristics, with permeabilities ranging from 9x10(-15) to 2x10(-9)m(2). The fault structures used in the model are simplified to nine faults that are laterally extensive or host significant fluid flow. These faults, other than the caldera collapse structures, strike northeast-southwest, reflecting the dominant structural trend in the TVZ. By visualising hydrogeological groups in 3D, realistic geology and hence permeability input data can be more easily integrated into numerical fluid flow models.
机译:我们介绍了陶波中部火山带(TVZ)的3D水文地质模型,包括七个地热田。结合井眼数据,地表地质和结构,可以生成深部代表性的地质组。模型区域中的地质单元主要根据具有相似水力特征的岩石类型被分为七个水文地质组,渗透率范围从9x10(-15)到2x10(-9)m(2)。模型中使用的断层结构简化为横向扩展或具有大量流体流动的9个断层。除火山口塌陷结构外,这些断层还向东北-西南方向移动,反映了TVZ的主要结构趋势。通过在3D中可视化水文地质组,可以更轻松地将现实地质以及渗透率输入数据集成到数值流体模型中。

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