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XDT on Geothermal Exploration
Understand Seismology, and you’ll
Understand the Subsurface
You don’t need to drill to know what's going on
beneath your feet. XDT uses passive seismic
signals to accurately describe the subsurface.
XDT has great experience with few staff. Therefore, we
can offer expert services at low costs.
Ph.D. – University of Washington, 1989
B.S. - University of Illinois, 1979
Seismologist and Volcanologist, Dr.
Jonathan Lees knows earthquakes
B.S. – North Carolina State
University
Alex Miller blends environmental
science with geophysics.
Geothermal exploration is more than
finding where the heat is. Its finding
the best way to it.
Subsurface
Structures
Subsurface
Densities
Fissures
and
Anisotropy
Rock Types
XDT provides innovative and proven
techniques of analysis. There aren’t any
black boxes here.
Shear wave splitting – can be used in identifying fissures and
other anisotropic elements. Click the earthquake circle below.
Earthquake
Seismometers
Subsurface cracks
and fissures
When the shear waves generated from the earthquake
propagate through the cracks, polarization occurs. The
different arrival times from the split s-waves can be
measured to model where the foliation or fissures occur.
Wave Attenuation and Velocity – used to identify subsurface
characteristics. Click the earthquake circle below.
Earthquake
Seismometers
Subsurface Body
When passive seismic waves propagate through differing
bodies, attenuation and changes in velocity occur. The
different arrival times and amplitudes can be measured to
model the properties and locations of the subsurface bodies.
Not only are our techniques innovative,
but our software is one of a kind.
Radiation
Patterns
Filtering
Spherical Distribution
Graphing
Focal Mechanism
Plotting
Interactive Maps
Arrival Time
Predictions
Time Series
analysis
Spectrograms
Seismic Tomography
Deconvolution
Cross Sections
Great Circles
Zoeppritz EquationsTomographic Inversion
Tomography
Ternary Plots
Area Analysis
Seismic Data
Conversions
Moveout
Displays
Want to know what’s going on in Enhanced
Geothermal Systems (EGS)? Show us the seismic.
Granite Body
Fissures/Cracks
Geothermal
Source
Seismometers
Upcoming Geothermal Projects? Give
us a call, we’re interested.
Alex Miller
Email: ajcmiller@xdtek.com
Phone: (919) 624-1251
Skype: alex_levi_miller
Jonathan Lees
Email: jonathan.lees@unc.edu

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Geo Explor

  • 1. XDT on Geothermal Exploration Understand Seismology, and you’ll Understand the Subsurface
  • 2. You don’t need to drill to know what's going on beneath your feet. XDT uses passive seismic signals to accurately describe the subsurface.
  • 3. XDT has great experience with few staff. Therefore, we can offer expert services at low costs. Ph.D. – University of Washington, 1989 B.S. - University of Illinois, 1979 Seismologist and Volcanologist, Dr. Jonathan Lees knows earthquakes B.S. – North Carolina State University Alex Miller blends environmental science with geophysics.
  • 4. Geothermal exploration is more than finding where the heat is. Its finding the best way to it. Subsurface Structures Subsurface Densities Fissures and Anisotropy Rock Types
  • 5. XDT provides innovative and proven techniques of analysis. There aren’t any black boxes here.
  • 6. Shear wave splitting – can be used in identifying fissures and other anisotropic elements. Click the earthquake circle below. Earthquake Seismometers Subsurface cracks and fissures When the shear waves generated from the earthquake propagate through the cracks, polarization occurs. The different arrival times from the split s-waves can be measured to model where the foliation or fissures occur.
  • 7. Wave Attenuation and Velocity – used to identify subsurface characteristics. Click the earthquake circle below. Earthquake Seismometers Subsurface Body When passive seismic waves propagate through differing bodies, attenuation and changes in velocity occur. The different arrival times and amplitudes can be measured to model the properties and locations of the subsurface bodies.
  • 8. Not only are our techniques innovative, but our software is one of a kind. Radiation Patterns Filtering Spherical Distribution Graphing Focal Mechanism Plotting Interactive Maps Arrival Time Predictions Time Series analysis Spectrograms Seismic Tomography Deconvolution Cross Sections Great Circles Zoeppritz EquationsTomographic Inversion Tomography Ternary Plots Area Analysis Seismic Data Conversions Moveout Displays
  • 9. Want to know what’s going on in Enhanced Geothermal Systems (EGS)? Show us the seismic. Granite Body Fissures/Cracks Geothermal Source Seismometers
  • 10. Upcoming Geothermal Projects? Give us a call, we’re interested. Alex Miller Email: ajcmiller@xdtek.com Phone: (919) 624-1251 Skype: alex_levi_miller Jonathan Lees Email: jonathan.lees@unc.edu