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Presentation - UC Davis Geology

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Identifying Blind Geothermal Systems through<br />

Integrated Geologic, Geochemical,<br />

and Geophysical Studies<br />

James Faulds, UNR<br />

Nevada Bureau of Mines & <strong>Geology</strong><br />

• Basin and Range – Region of high heat flow<br />

• Ironic that what little water region has is hot<br />

• Difficult to find sufficient fluid flow<br />

• Permeability more important than temperature<br />

• Most geothermal resources are blind<br />

• Need multi-disciplinary studies to discover new<br />

resources<br />

Desert Peak – Blind System


Challenges, Barriers, and Needs<br />

• Current technology cannot identify best<br />

geothermal sites with a high degree of<br />

certainty without drilling.<br />

– Permeability<br />

– Temperature<br />

• Drilling is expensive and generally has high<br />

risks.<br />

• Inadequate knowledge precludes low-risk<br />

options to effectively select sites and<br />

characterize their physical parameters as<br />

potential geothermal reservoirs before<br />

drilling.<br />

• Better characterization of known systems<br />

needed to address these problems.<br />

• Our approach – Characterize settings<br />

favorable for geothermal activity and develop<br />

more comprehensive, conceptual models that<br />

can facilitate exploration.<br />

Beowawe<br />

Fly Ranch Geyser – Blind system


Exploration Challenges<br />

• Exploration Challenges<br />

– Spring directly above upflow from<br />

deep source (uncommon)<br />

– Outflow from source (common)<br />

– Hidden or blind systems (most<br />

common)<br />

• Results – significant drilling risk<br />

– Hot dry wells<br />

– Overturn in down-hole temperatures<br />

• Need better conceptual models to:<br />

– Locate areas of upflow<br />

– Avoid typically less productive<br />

outflow zones<br />

Non-Productive Well<br />

Blue Mt., Nevada<br />

Productive Well<br />

Productive wells commonly proximal<br />

to non-productive wells<br />

Productive<br />

Non-Productive Well<br />

Productive Well<br />

Non-Productive<br />

Non-Productive<br />

Desert Peak, Nevada<br />

From Richards and<br />

Blackwell, 2002


Project Goals<br />

Gravity Data<br />

Geologic-Structural Data<br />

• Identify multi-faceted characteristic<br />

signature of known, high-enthalpy,<br />

productive geothermal systems based<br />

on several methods and techniques:<br />

– Structural geology and geologic maps<br />

– Gravity<br />

– Seismic reflection-refraction<br />

– Magnetotellurics (MT)<br />

– Soil gas flux<br />

– Geochemistry<br />

• Integrate data into one geodatabase<br />

• Generate 3D models of systems<br />

Magnetotelluric Data<br />

Seismic Reflection Data<br />

3D Model


Project Objectives<br />

• Determine characteristic geologic and<br />

geophysical signature for productive<br />

geothermal systems<br />

• Relate these findings to tectonic setting<br />

and regional strain rates<br />

• Later apply these methods in a Phase<br />

II to discovering blind geothermal<br />

systems<br />

– Estimates suggest that ~3/4 of systems in<br />

Great Basin region are blind or hidden<br />

– Example below from Hot Springs Mts, NW<br />

Nevada – 2 of 3 high-temp systems blind<br />

Structural Settings of Geothermal<br />

Systems (Faulds et al., 2013)


Approach<br />

• Review all available data sets for several<br />

operating geothermal systems in<br />

different structural settings<br />

• Integrate geologic, geophysical, and<br />

geochemical data from productive<br />

geothermal fields in Great Basin region,<br />

(e.g., systems with existing power plants):<br />

– Dixie Valley<br />

– Steamboat<br />

– Desert Peak<br />

• Phase I relies on existing data due to<br />

limited funding for data acquisition and<br />

is collaborative with industry at these<br />

sites<br />

• Very limited new data acquisition<br />

possible in some areas<br />

• Variety of settings selected for study to<br />

best characterize range of values for<br />

productive systems


• Integrated geodatabases<br />

contributed to NGDS.<br />

• Descriptions of characteristic<br />

signatures.<br />

• Final report.<br />

Outcome/Deliverables<br />

• Peer-reviewed published paper.<br />

Steamboat, Reno


Impact<br />

• Project has potential of making critical<br />

breakthroughs<br />

– Identifying characteristic signatures of<br />

geothermal systems<br />

– Developing techniques for identifying blind<br />

geothermal systems<br />

• May significantly expand the overall<br />

geothermal potential of the Great Basin<br />

• May lower costs of geothermal development<br />

• May foster economic development in rural<br />

areas<br />

• Project will help educate next generation of<br />

geothermal geoscientists<br />

Strain rates reflect the<br />

second invariant strain<br />

rate tensor (10 -9 /yr)<br />

Faulds et al. (2012)<br />

Fairway 3D Mapping of Geothermal System<br />

(Siler and Faulds, in press)


Project Duration/Proposed Budget<br />

• Project duration – October 1, 2013<br />

to September 30, 2014.<br />

• Proposed Budget - $59,990<br />

– Non state-funded faculty salaries - $11,000<br />

– Graduate student salaries - $30,000<br />

– Fringe – $8,240<br />

– Travel - $2,750<br />

– Operating - $2,000<br />

– Overhead (10%) - $6,000<br />

Neal Hot Springs, Oregon<br />

Temperature Anomaly,<br />

Desert Peak, NV


Questions?<br />

Please fill out Level of Interest Evaluation Form (L.I.F.E.)<br />

Roosevelt, Utah

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