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Title: www.unr.edugeothermal


1
www.unr.edu/geothermal
Resource Exploration, Assessment and
Research Lisa Shevenell, Mark Coolbaugh, Chris
Sladek, Rick Zehner, Chris Kratt GEA -
Geothermal Issues and Outlook Workshop October
4, 2008
2
Great
  • Focus
  • Applied Geoscience Research
  • Conventional Hydrothermal Systems
  • Collaboration w/DOE, Industry Navy
  • Education of Students for Workforce
  • Database Development, Maintenance and Serving on
    the Web

3
Assessment for Nevada
  • GRC Bull, June 2008 (Shevenell, Morris,
    Blackwell)
  • Preferred values _at_ known systems
  • Permits
  • Heat Loss
  • GeothermEx PIER
  • WGA
  • Nominal 5 MW assumption
  • Minimum 2170 MW _at_ 160 sites

4
New Exploration and Assessment Methods On-going
Research
  • Conducting regional studies to develop models and
    build geothermal potential maps local studies to
    better understand systems

5
Gravity, Dilation, T-grad, Seismicity
Coolbaugh, et al.
6
Detailed Mapping in Modern Plate Tectonic Context
Desert Peak
Overlapping Normal Faults
  • En echelon NNE normal faults
  • Subvertical conduits
  • High fracture density
  • Multiple step overs
  • Other favorable settings
  • Terminations of range-front faults (Gerlach)
  • Intermeshing opposing systems (Salt Wells)

Faulds
7
Recent discoveries of a number of previously
unknown geothermal systems in the Great Basin
suggest that a large undiscovered resource base
does in fact exist.
McGinness Hills Tungsten Mountain Astor
Pass Smoke Creek Desert Pyramid Rock Rhodes
Marsh Salt Wells north
8
Remote Sensing for mapping mineralogy and thermal
anomalies
Hymap 3-5 meter
Kratt, Calvin
9
ASTER delineates borates in SW Nevada
  • locate systems without hot springs issuing at
    surface

ASTER color Composite image
Kratt, Coolbaugh
10
Rhodes Marsh, Mineral County, NV. Red
strike slip fault Black normal fault
Soda Springs, 112 geotherm.
X
Active range front faulting
opalized sands
springs/wells
Warm well with borates 155 / 162
geotherm. sampled 2005
Coolbaugh, Kratt, Zehner, Sladek
11
New Assessment Methods Shallow Temperature
Surveys
Sladek, Zehner, Kratt, Coolbaugh, Penfield
12
Tungsten Mountain discovered during Au
exploration drilling in 2005,
2006 (information provided courtesy NewCrest
Resources, Tom Kilbey) - northwest side of
Edwards Creek Valley, Nevada - geothermal
system occupies possible step-over in range
bounding fault
  • All 23 exploration holes hit hot water, with
  • temperatures ranging from 50-95C, often with
    steam, at
  • depths of 90-275 m
  • Hot water encountered over 2 km strike length,
    open in
  • all directions
  • - Geothermometers 174C Na-K-Ca-Mg 177C quartz

13
Kratt, Zehner, Penfield
14
Teels Marsh December 2007
Kratt, Zehner, Penfield
15
Temperatures (C) From Cold Springs
16
New Discoveries
  • Astor Pass RS, TS
  • Blue Mountain GE
  • Bonham Ranch RS, TS
  • McGinness Hills GE
  • Rhodes Marsh RS, TS
  • Salt Wells (better defined) TS
  • Teels Marsh RS, TS
  • Tungsten Mountain GE, TS

GE Gold Exploration RS Remote Sensing
TS Temperature Surveys
17
Proposed Work
  • 4 current proposals
  • 2 in the process of award
  • Sites Aurora, BR 16, Colado, Cove Fort,
    Hawthorne, Lee-Allen, NY Canyon, Patua, Salt
    Wells, Stillwater, Surprise Valley
  • Sponsors
  • Enel, North America
  • Navy GPO
  • NREL
  • Vulcan

18
Proposed Work
  • Data gathering, assimilation, GIS
  • Evaluate active faulting - LSA photography
  • GPS to assess geothermal targets modeling
    crustal stress
  • EQ Monitoring
  • Field Recon

19
Proposed Work
  • Geochemistry
  • Mapping geothermal features
  • Rock characterization rock mechanics
  • 3-D Seismic
  • Shallow T-surveys
  • Structural mapping and analysis

20
Conclusions
  • Research has enabled the development of
    significant new evaluation and exploration tools
  • New tools helping to identify new geothermal
    resources and better assess existing ones
  • Undiscovered resource base in the GB is
    significant but unknown need assessment
  • Geothermal energy has the potential to be a major
    contributor to renewable energy portfolios in NV

21
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22
Silicified sediments (opal)
All blind geothermal systems in Nevada that
are currently producing electricity have some
surface signatures
Carbonate tufa/travertine
Clay alteration
Borate and sulfate evaporites
23
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