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Developing Systematic Workflow From Field Work to Quantitative 3D Modeling for Successful Exploration of Structurally Controlled Geothermal Systems

机译:开发从现场工作到定量3D建模的系统工作流程,以成功探索结构受控的地热系统

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Ongoing research has shown that structurally controlled geothermal systems are associated with specific structural settings, such as terminations of major normal faults, accommodation zones, pull-aparts in strike-slip faults, displacement transfer zones, or step-overs in range-front faults. The structural framework of each of these principal structural settings is innately complex, and the permeable and productive areas are commonly spatially discrete, limited in some cases to a single part of an individual fault zone. Successful development of these systems relies on accurately defining these permeable up-flow zones in 3D space for precise well targeting and resource estimation. However, there is no single tool that can both define the detailed structural framework of a geothermal area and also define the individual parts of which faults currently host the geothermal fluids. Through recent and ongoing detailed studies of over 20 systems in the Great Basin region, we have been developing a systematic workflow that integrates multiple geologic and geophysical data sets. The workflow is centered on constructing an accurate and detailed 3D geologic map while using the same conventional geologic reasoning as is used in constructing 2D geologic cross-sections and maps of the ground surface. The 3D geologic map is then used to run quantitative 3D models, consider discrete geothermal indicator data sets relative to the entire 3D map, define a conceptual fluid-flow model, and select well targets.
机译:正在进行的研究表明,结构受控的地热系统与特定的结构设置相关,例如主要正断层的终止,调节带,走滑断层中的拉脱,位移传递带或范围前断层中的阶跃。这些主要结构设置中的每一个的结构框架本来就是复杂的,并且可渗透和生产性区域通常在空间上是离散的,在某些情况下限于单个断层带的单个部分。这些系统的成功开发依赖于在3D空间中准确定义这些可渗透的向上流动区域,以进行精确的井眼定位和资源估算。但是,没有一个单一的工具既可以定义地热区域的详细结构框架,又可以定义当前包含地热流体的断层的各个部分。通过对大盆地地区20多个系统的最新和正在进行的详细研究,我们一直在开发一种集成了多个地质和地球物理数据集的系统工作流程。工作流程的重点是构建准确而详细的3D地质图,同时使用与构造2D地质剖面和地面图相同的常规地质推理。然后使用3D地质图运行定量3D模型,考虑相对于整个3D地图的离散地热指标数据集,定义概念性流体流动模型,并选择井目标。

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