Three-dimensional geologic mapping to assess geothermal potential: examples from Nevada and Oregon

Abstract Geologic structure plays an important role in controlling fluid flow in geothermal systems. In particular, very complex structural settings, consisting of many closely spaced and intersecting faults, host many geothermal systems. To elucidate the key geologic factors that affect fault-contr...

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Main Authors: Drew L. Siler, James E. Faulds, Nicholas H. Hinz, Gregory M. Dering, Joel H. Edwards, Brett Mayhew
Format: Article
Language:English
Published: SpringerOpen 2019-01-01
Series:Geothermal Energy
Online Access:http://link.springer.com/article/10.1186/s40517-018-0117-0
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spelling doaj-d35e2df0ba454753b1dc2d79af36c0152020-11-25T01:44:07ZengSpringerOpenGeothermal Energy2195-97062019-01-017113210.1186/s40517-018-0117-0Three-dimensional geologic mapping to assess geothermal potential: examples from Nevada and OregonDrew L. Siler0James E. Faulds1Nicholas H. Hinz2Gregory M. Dering3Joel H. Edwards4Brett Mayhew5U.S. Geological SurveyNevada Bureau of Mines and Geology, University of Nevada, RenoNevada Bureau of Mines and Geology, University of Nevada, RenoNevada Bureau of Mines and Geology, University of Nevada, RenoNevada Bureau of Mines and Geology, University of Nevada, RenoNevada Bureau of Mines and Geology, University of Nevada, RenoAbstract Geologic structure plays an important role in controlling fluid flow in geothermal systems. In particular, very complex structural settings, consisting of many closely spaced and intersecting faults, host many geothermal systems. To elucidate the key geologic factors that affect fault-controlled geothermal circulation, it is critical to precisely characterize the structural and stratigraphic geometries in these complex settings. Here, we present a methodology and the results of 3D geologic analyses of two geothermal systems in the Basin and Range, USA. This methodology is a quantitative and geologically focused technique that can be used to precisely characterize geothermal areas, in a time when future geothermal growth demands increased exploration precision and efficiency. Surficial and subsurface geologic and geophysical data are synthesized in the construction of detailed 3D geologic maps of geothermal areas. Based on these 3D geologic maps, we examine several geologic attributes that control permeability development and geothermal fluid flow along faults. We use the stress state of faults and the distribution of structural discontinuities (i.e., fault intersections and fault terminations) to identify locations of upflow along faults in these geothermal systems. These results and the methodology presented herein are directly applicable to structurally controlled geothermal fields in the Basin and Range and worldwide. As development focus shifts toward blind geothermal resources, integration of precisely characterized subsurface structural information into exploration methods will be increasingly critical to continued growth in geothermal exploration and development.http://link.springer.com/article/10.1186/s40517-018-0117-0
collection DOAJ
language English
format Article
sources DOAJ
author Drew L. Siler
James E. Faulds
Nicholas H. Hinz
Gregory M. Dering
Joel H. Edwards
Brett Mayhew
spellingShingle Drew L. Siler
James E. Faulds
Nicholas H. Hinz
Gregory M. Dering
Joel H. Edwards
Brett Mayhew
Three-dimensional geologic mapping to assess geothermal potential: examples from Nevada and Oregon
Geothermal Energy
author_facet Drew L. Siler
James E. Faulds
Nicholas H. Hinz
Gregory M. Dering
Joel H. Edwards
Brett Mayhew
author_sort Drew L. Siler
title Three-dimensional geologic mapping to assess geothermal potential: examples from Nevada and Oregon
title_short Three-dimensional geologic mapping to assess geothermal potential: examples from Nevada and Oregon
title_full Three-dimensional geologic mapping to assess geothermal potential: examples from Nevada and Oregon
title_fullStr Three-dimensional geologic mapping to assess geothermal potential: examples from Nevada and Oregon
title_full_unstemmed Three-dimensional geologic mapping to assess geothermal potential: examples from Nevada and Oregon
title_sort three-dimensional geologic mapping to assess geothermal potential: examples from nevada and oregon
publisher SpringerOpen
series Geothermal Energy
issn 2195-9706
publishDate 2019-01-01
description Abstract Geologic structure plays an important role in controlling fluid flow in geothermal systems. In particular, very complex structural settings, consisting of many closely spaced and intersecting faults, host many geothermal systems. To elucidate the key geologic factors that affect fault-controlled geothermal circulation, it is critical to precisely characterize the structural and stratigraphic geometries in these complex settings. Here, we present a methodology and the results of 3D geologic analyses of two geothermal systems in the Basin and Range, USA. This methodology is a quantitative and geologically focused technique that can be used to precisely characterize geothermal areas, in a time when future geothermal growth demands increased exploration precision and efficiency. Surficial and subsurface geologic and geophysical data are synthesized in the construction of detailed 3D geologic maps of geothermal areas. Based on these 3D geologic maps, we examine several geologic attributes that control permeability development and geothermal fluid flow along faults. We use the stress state of faults and the distribution of structural discontinuities (i.e., fault intersections and fault terminations) to identify locations of upflow along faults in these geothermal systems. These results and the methodology presented herein are directly applicable to structurally controlled geothermal fields in the Basin and Range and worldwide. As development focus shifts toward blind geothermal resources, integration of precisely characterized subsurface structural information into exploration methods will be increasingly critical to continued growth in geothermal exploration and development.
url http://link.springer.com/article/10.1186/s40517-018-0117-0
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