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From Creekology to Rocket Science:
The Evolution of Remote Sensing/GIS
     in Oil and Gas Exploration
           A Presentation for

         2011 Texas GIS Forum
             October 26, 2011
              Austin, Texas

              David G. Koger

                Fort Worth
Becoming an Expert
   takes 10,000 hours, timing & luck
Becoming an Expert
 takes 10,000 hours, timing & luck
 and the desire to show up
Becoming an Expert
 takes 10,000 hours, timing & luck
 the desire to show up

 and learning “dialogues of business”
Becoming an Expert
 takes 10,000 hours, timing & luck
 the desire to show up

 and learning “dialogues of business”

 and learning after school‟s out
Becoming an Expert
 takes 10,000 hours, timing & luck
 the desire to show up

 and learning “dialogues of business”

 and learning after school‟s out

 e.g. the expert mortician
Creekology: Seeing into the Earth
Creekology: Seeing into the Earth

   „Seepology‟...Native Americans
    extracted medicinal goo
   The first oil wildcatters drilled at the
    bends in streams
   Early USGS maps showed rough
    stream drainage patterns
Creekology
   Satellite data—large scale and highly
    accurate—merged creekology with
    geology.
   Photogeologic work was now possible
    without troublesome mosaicking.
   Remotely sensed data are spatially and
    spectrally better than airphotos, and has
   A greater variety of sun angles, moisture
    conditions, and seasonal samplings.
How this will work
   Agenda:
    • Part 1: Case studies (natural disasters;
      environmental; damages & liabilities;
      exploration; logistical support)
    • Part 2: Photogeology; how images work
    • Part 3: Field work: it costs a lot.
      Getting better data; saving time and
      money on your surveys
    • Part 4: Other stuff to know, time
      permitting
Part 1: Case Studies
 ...Liabilities, Damages,
     Operations and
      Planning…
Case study #1
   Put it back the way you found it.
(not an unreasonable request…)
   What is a weed, after all?
(everybody knows what a weed is, right?)
 Causing damage to the bushes
 and what‟s beneath the bushes
  (USLE).
 Putting it back
(how hard can that be?)
Case study #1
   Put it back the way you found it.
(not an unreasonable request…)
   What is a weed, after all?
(everybody knows what a weed is, right?)
 Causing damage to the bushes
 and what‟s beneath the bushes
  (USLE).
 Putting it back
(how hard can that be?)
Case study #1
   Put it back the way you found it.
(not an unreasonable request…)
   What is a weed, after all?
(everybody knows what a weed is, right?)
 Causing damage to the bushes
 and what‟s beneath the bushes
  (USLE).
 Putting it back
(how hard can that be?)
Case study #1
   Put it back the way you found it.
(not an unreasonable request…)
   What is a weed, after all?
(everybody knows what a weed is, right?)
 Causing damage to the bushes
 and what‟s beneath the bushes
  (USLE).
 Putting it back
(how hard can that be?)
Case study #1
   Put it back the way you found it.
(not an unreasonable request…)
   What is a weed, after all?
(everybody knows what a weed is, right?)
 Causing damage to the bushes
 and what‟s beneath the bushes
  (USLE).
 Putting it back
(how hard can that be?)
Case study #2
 300,000 acres burned up
 Whose land was damaged?

 What portions were grassland, crops,

  trees?
 Where‟d the fire actually start?

 Who‟s responsible?
Mapping Wildfire
Wildfire 6 hrs later
Wildfire Damage Outline...LS5
Wildfire Burn Severity
Fire Severity on Property
       Boundaries
High Water Marks
Creating up-to-date
 information.

A word about coastlines, tides,
 erosion (and where the fish
 are).
Freshwater or Ocean; currents and
  thermal differences for fishing
Exploration Examples
 Nebraska
 Fayetteville Shale

 Marcellus Shale

 Romania

 Paraguay

 Costa Rica

 Kansas DOE three times
Exploration Examples
 Nebraska
 Fayetteville Shale

 Marcellus Shale

 Romania

 Paraguay

 Costa Rica

 Kansas DOE three times
Large-scale Data Management:
   Photogeology Mapping of Nebraska

The goal was
to foment
exploration, so
we conducted
a
photogeology
study of
Nebraska at
medium scale,
using satellite
imagery,
gravity and
magnetics.
Large-scale Data Management:
   Photogeology Mapping of Nebraska


We acquired
topographic
maps at
1:250,000 and
1:100,000
scales) for
spatial
reference with
the satellite
imagery.
Large-scale Data Management:
   Photogeology Mapping of Nebraska



Structural
interpretations
were made
from and
overlaid onto
the imagery.
Large-scale Data Management:
   Photogeology Mapping of Nebraska


The
interpretations
were overlaid
onto topo
maps to
provide a
universal map
reference
display.
Large-scale Data Management:
   Photogeology Mapping of Nebraska



A merge of
imagery, map,
and
interpretation.
Exploration Examples
 Nebraska
 Fayetteville Shale

 Marcellus Shale

 Romania

 Paraguay

 Costa Rica

 Kansas DOE three times
Landsat
  bands 7, 4,
       and 2;
 composited
  as color on
the following
         slide
Landsat
composites
from two
different
dates. Also,
the
geometry
differs.
Regional (250K+) Interpretations
Regional + Local (24K)
   Interpretations
Exploration Examples
 Nebraska
 Fayetteville Shale

 Marcellus Shale

 Romania

 Paraguay

 Costa Rica

 Kansas DOE three times
Exploration Examples
 Nebraska
 Fayetteville Shale

 Marcellus Shale

 Romania

 Paraguay

 Costa Rica

 Kansas DOE three times
Romania
   Identify features of exploration
    interest (e.g. fault/frax, structures,
    tonal anomalies)

   Update WWII-era maps

   Identify high-cost damage areas
    (e.g. vineyards....)
Data Types & Sources: Multi-sensor merge
           (Landsat + SPOT)




  The area had only WWII-era maps....
Data Types & Sources: Multi-sensor merge
            (Landsat + SPOT)




This is the 5-meter panchromatic SPOT image that supplied
the spatial detail in the study, while 28.5m Landsat data
provided the spectral information.
Data Types & Sources: Multi-sensor merge
           (Landsat + SPOT)




The multi-band Landsat was encoded to hue and
saturation, while the higher resolution SPOT was
assigned to intensity.
Data Types & Sources: Multisensor merge
           (Landsat + SPOT)




 The photogeology interpretations are overlaid.
Data Types & Sources: Multisensor merge
           (Landsat + SPOT)
Data Types & Sources: Multisensor merge
           (Landsat + SPOT)
Exploration Examples
 Nebraska
 Fayetteville Shale

 Marcellus Shale

 Romania

 Paraguay

 Costa Rica

 Kansas DOE three times
Paraguay Information Needed
Where are existing roads that can be used
 for moving equipment and laying out field
 work equipment,

Where are the tracks of previous field work?

Update maps...collect detailed knowledge of
 the area,

Find water sources: rivers, ponds, springs.
Gold = Your New, Geometrically
      Accurate Roadmap
Exploration Examples
 Nebraska
 Fayetteville Shale

 Marcellus Shale

 Romania

 Paraguay

 Costa Rica

 Kansas DOE three times
Stress-Strain Ellipsoid
Compression at 100K Scale
Stress-Strain @6K Scale
Exploration Examples
 Nebraska
 Fayetteville Shale

 Marcellus Shale

 Romania

 Paraguay

 Costa Rica

 Kansas DOE three times
“Remote Sensing Image Analysis
    Toward Understanding
   Sequestration Potential of
      Southern Kansas”
  DE-FE0002056 – “Modeling CO2 Sequestration in Saline
Aquifer and Depleted Oil Reservoir to Evaluate Regional CO2
  Sequestration Potential of Ozark Plateau Aquifer System,
                   South-Central Kansas”

                            by
                     David G. Koger
                   Ralph N. Baker, PhD
                         Fort Worth
Information needed:
   Is it safe to inject CO2?

   Will it come back up?

   How quickly?

   Where?

   Where might it get trapped?

   What are the cost trade-offs?
Remote Sensing to the Rescue

• Help map the subsurface
   Conduits / Compartments;
   Migration fairways / Sealing mechanisms




• Define structural & stratigraphic
  elements
     these affect Fluid Movement
(Information, continued)

All of which supports:
 Environmental Risk Analysis
 and
 Helps determine reservoir
 suitability for CO2 storage
Because knowing the contrasts of
    Conduits vs. Compartmentalization
                       and
  Migration Pathways vs. Sealing Factors

 Must be understood & modeled to predict
  Fluid Movement and reservoir integrity
          because this is how we can know
     how and where groundwater flows
                  and, therefore,
How/if CO2 injections might affect the water
 table (e.g. we expect some CO2 leakage
 along fractures; high porosity/permeability
 zones are especially noteworthy….
Regional Gravity & Magnetics




   Define Major Basement Block Boundaries, Structural Grain
Regional Gravity & Magnetics




   Define Major Basement Block Boundaries, Structural Grain
Regional Satellite Photogeology
Local on top of Regional
Exploration Examples
 Nebraska
 Fayetteville Shale

 Marcellus Shale

 Romania

 Paraguay

 Costa Rica

 Kansas DOE three times
“Remote Sensing Image Analysis of the
        Bemis-Schutts Field,
       Ellis County, Kansas”
        in support of U.S. Dept of Energy/KS Geological Survey’s
DE-FE0004566 – “Prototyping and testing a new volumetric curvature tool for
 modeling reservoir compartments and leakage pathways in the Arbuckle
  saline aquifer: reducing uncertainty in CO2 storage and permanence”

                                    by
                        David G. Koger
                      Ralph N. Baker, PhD
                    Koger Remote Sensing, Fort Worth
Stress/Strain Model
Regional-scale work
Local-Scale work
Local-scale interpretations
How this will work
   Agenda:
    • Part 1: Case studies (natural disasters;
      environmental; damages & liabilities;
      exploration; logistical support)
    • Part 2: Photogeology; how images work
    • Part 3: Field work: it costs a lot.
      Getting better data; saving time and
      money on your surveys
    • Part 4: Other stuff to know, time
      permitting
How satellites work:
   They collect their data with
    scanners. Other scanners are:
     • video cameras,
     • fax machines,
     • barcode readers,
     • Magnetic Resonance Imaging
       machines,
     • video game characters‟ vision...
Part 2 (how images work)

   About satellite data
    • How it collects & organizes data
    • Attributes of these data
         Spectra, spatial, temporal
   Photogeology for exploration
Part 2 (how images work)

   About satellite data
    • How data are collected & organized
    • Attributes of these data
        Spectra, spatial, temporal


   Photogeology for exploration
WorldView-2
Docks and Cranes pre-quake
Docks and Cranes Collapsed in
     Water (after quake)
Presidential Palace, post-quake
Relief Supplies Arrive
Haiti Damage Severity Map
Part 2 (how images work)

   About satellite data
    • How it works
    • Attributes
         Spectra, spatial, temporal
   Photogeology for exploration
ROY G BIV
Digital Image Processing

“Pixel” =
  “picture
  element”
  ...one
  spatial
  unit plus
  the
  spectra.
Part 2 (how images work)
   About satellite data
    • How it works
    • Attributes
         Spectra, spatial, temporal
   Photogeology for exploration
Landsat TM footprint
Reducing Data to Information
A typical project area encompasses:

•2-6 Landsat scenes (600MB to 1.8 GB raw data)
•12-36 USGS raster topo sheets (500 Mb to 1.5 Gb)
•Ancillary magnetics and gravity surveys (200 MB)
•High resolution aerial imagery (800MB to 2 GB)

For a total of 2.1 to 5 GB of raw data

Color composites, PCAs, structural interpretations, and ancillary
data can make 12-15 GB of additional files

All this fuss over data selection, processing, and analysis is
because the process must deliver the information needed to
make decisions.
Landsat TM processing

Landsat Band 7 raw data




with brightness and
contrast stretches
applied
Landsat TM processing


Same area: Band 1 raw data




       stretched
Landsat TM processing


Band 3-2-1 composite of
raw data




   Same, stretched
Landsat TM processing


Band 7-5-4 composite of
raw data




   Same, stretched
Landsat TM processing




Multitemporal Principal Components Analysis
        (or De-correlation Stretch).
Spatial Resolution…detail
Part 2

   About satellite data
    • How it works
    • Attributes
         Spectra, spatial, temporal
   Photogeology for exploration
At left, March 12 shows vegetation patterns in
the early spring (bright greens).

     At right, December 23 vegetation is dormant.

Both images are “true.”
Palo Pinto Landsat multi-temporal comparisons




              September

              and March
Multi-temporal 1m data comparison
     for tax appraisal purposes
Part 2
   About satellite data
    • How it works
    • Attributes
         Spectra, spatial, temporal
   Photogeology for exploration
You can never have too
  much information

What you do have:
  production trends,
  a regional framework,
  well logs here and there, and
  maybe some field work.
Available information is massive:
 Surface and subsurface geology maps
 Current and historic well logs

 Topographic maps

 Seismic analyses

 Gravity surveys

 Magnetic surveys

 Satellite and aerial imagery

 Geochem surveys
The ideal tool would:
1) fill in every empty space of the
   mosaic
2) highlight anomalous conditions,
   and map structure: large folds and
   astroblemes or localized fracturing
   and reefs.
An even better tool would:
a) sample at intervals in time
 (all seasons, wet and drought
 conditions, over decades),
 and
b) offer adaptive scale to
 support either frontier or
 mature basin analysis.
Two Kinds of Tools:
•   Those that find structure
•   Those that find anomalous
    conditions


Remote sensing does both
The Crust of Earth is:

•   Thin, unstable, and floats
•   Bombarded with energy daily
•   Generates soil @ 3 tons per acre
    per year
•   Washed down and compacted daily
Remote sensing photogeology
is a blend of several disciplines:

      optics
      physics

      electronics

      cartography

      natural science

      computer sciences
Patterns: Their causes and effects

Subsurface activity imprints the
 surface for many reasons :

 constant micro-earthquakes,
 settling,

 erosion,

 micro-seepages.
Microbes are everywhere!
 We are 1/10
                th us; 9/10th microbes.

 H.pylori causes 90% of peptic ulcers.

 Antibiotics fight harmful microbes.

 Yogurt has good ones.

 They‟re in amber, meteorites, Mars rocks,

  and 250 million-yr-old crystals.
 A billion microbes in 1 gram of topsoil.

 Dead microbes make topsoil.

 Other microbes clean up oil spills.

 A trillion are on each of your feet.
Healthy topsoil…
 retains water better,

 resists erosion,

 has more oxygen,

 better nutrients,

 Microbes and earthworms like it,

 compacts less, and

 is friendlier to roots.
Hydrocarbon-eating microbes
 Thrive above oil and gas reservoirs.
 Create a magnetic residue.

 Are counted.

 Deplete oxygen in soil.

 Do not build good soil.

 Seeps are mostly vertical; dynamic.

These conditions have been
  recorded for 39 years....
Finding Structure: Astrobleme
Astrobleme with magnetics
The Information in Photogeology
Lineaments:
Faults, fractures, fracture orientation and joints can
  have surface expression as:
 Linear escarpments. Changes in the directions
  they face can mean strike-slip faults.
 Linear and right angle bends in drainage courses.

 Drainages running in parallel.

 Aligned drainages on opposing sides of a drainage
  divide.
 Tributaries entering main streams in direct
  opposition.
 Moisture accumulation in linear patterns; alignment
  of water bodies
The Information in Photogeology
Lineaments (continued):
 Linear vegetation patterns due to water
  availability.
 Aligned notches on ridge crests.

 Subtle dip changes, varying lithologies or
  changes in rock texture.
 Variation in thermal signature.
 Large topographic trends align with
  basement lineaments.
 High fracture densities enhance
  hydrocarbon mobility at depth
The Information in Photogeology
Positive Structures at Depth can appear as…
 Surface tonal anomalies.

 Circular features can indicate buried structure.

 Vegetation differences: health, leaf water content,
  population distribution.
 Differential compaction, loading, increased fracture
  density over and adjacent to buried structure.
 Soil color and texture alterations…staining, bleaching,
  cobbling.
 Local, slight topographic highs or lows.

 Subtle variations in moisture accumulation on the
  flanks of buried structure.
Mapping and GIS: making it all fit

Google Earth: “cans” and “can’ts”:
Very popular new web tool;
   •Fast and easy for finding places and routes
   •Reasonably accurate cartographic information;
   •High resolution imagery in some locations;
   •Excellent 3D visualization tool
However:
   •Not accurate enough to be used as an exploration map
   •Image dates unknown
   •Most areas outside cities and large towns in low resolution
   •Color imagery not good enough for photogeologic analysis
How this will work
   Agenda:
    • Part 1: Case studies (natural disasters;
      environmental; damages & liabilities;
      exploration; logistical support)
    • Part 2: Photogeology; how images work
    • Part 3: Field work: it costs a lot.
      Getting better data; saving time and
      money on your surveys
    • Part 4: Other stuff to know, time
      permitting
Field Work
    Support
Requires Leadership…
Knowing where you‟re
       going….
Field Work Support in Three Parts

1) Strategies to get you the best
   possible data

2) Logistical hoops to jump through
   ($), and

3) Tools that will help you
Wait a second: has your
area been shot already?

  “Earth Detective” work on
  an unusual application for
    (free) satellite data....
Has your area been shot?
 Google Earth
 Landsat 5

 Landsat 7

 Airphotos in archive

    • Military
    • DOT
    • USDA
    • Farm Service
Has the area been shot?
   The trouble with airphoto coverage:
    • it is spotty
    • often monochromatic
    • often mono-temporal
   Satellite data
    •   have an archive that goes back 29 years
    •   they‟re inexpensive…mostly free
    •   they cover 10,000 square miles
    •   you get to choose:
            the right sun angle
            the right soil moisture
            the right vegetation cover
No shoots as of 29Jan95
No shoots as of 21Oct05
No shoots as of 30Oct08
No shoots as of 29Nov09
Has the area been shot?
   The trouble with airphoto coverage:
    • it is spotty
    • often monochromatic
    • often mono-temporal
   Satellite data
    •   have an archive that goes back 29 years
    •   they‟re inexpensive…mostly free
    •   they cover 10,000 square miles
    •   you get to choose:
            the right sun angle
            the right soil moisture
            the right vegetation cover
Yes, there were shoots in the area
          as of 18July06
Only six months later, seeing it is
difficult due to the low sun angle:
What you should know about
         supporting field work
   Somebody is responsible. Apparently, it‟s you.
   Good information won‟t just happen…it demands
    good planning.
   List all the things that can go wrong in the field.
    Plan for them.
   Field work is expensive. Your project will go over
    budget unless good information supports your
    plan....
   Collecting the best quality field data results from
    a good plan.
Field work Support in Three Parts

1) Strategies to get you the best
   possible data

2) Logistical hoops to jump through
   ($), and

3) Tools that will help you
The Subsurface

   ...is where the
 treasure—water or
oil—is: how can we
  see down there?
On the Geology Side:
Expensive subsurface surveys are useless
  unless they produce a proper image of the
  subsurface.
Advanced modeling—before the shoot
 design—of the strata below will dictate
 your:
  • receiver and source spacing,
  • the location and spacing of lines
  • the geometric organization of the signal source
    and receiver locations, i.e. the design.
Magnetics:
“basement topography”
Regional Drainages
Topo on DEM
Satellite data on DEM: slippery slopes
Surface composition: i.e. slippery soils
The Subsurface in 3-D
   Generate a model of the earth at depth
    using:
     • surface & subsurface structure maps,
     • velocity information, and
     • other seismic data.
   Ray tracing from the target horizons will
    identify your optimum shoot parameters
3-D Earth Model
Initial Design
 Test it to ensure that subsurface
  coverage is not compromised.
 A full patch, 3D ray tracing shows:

    • which parameters will best image your
      target.
   3-D ray tracing may be re-run after
    “no permit areas” or other obstacles
    are found.
3-D Ray Tracing
Final Design
   Subsurface model is in place
   Offset sources & receivers have been ray
    traced in the model
   Hazards are identified
   Protocol for handling offsets is established
   …meaning: geophysical decisions are not
    left to the field crew
   We‟re now ready to go to the field
Field Support in Three Parts

1) Strategies to get you the best
   possible data

2) Logistical hoops to jump through
   ($), and

3) Tools that will help you
Knowing What’s in
  Real World…
 Dealing with it.
Realities of Designing Field Work
 The goals of field work and land
  owners are often in conflict.
 It takes knowledge, effort, and time,

  to:
    • identify the project‟s requirements and
    • endure the permitting process.
   A third party consultant will save you
    time and money.
Two Costly Philosophies
   Being Rigorous:
    • a strict technical design w/o regard for
      obstacles on the ground…
    Your field personnel have to deal with whatever
      obstacles they encounter.
   Being Serendipitous:
    • personnel are sent to the field w/no
      coordination...
    They wander around—on your dime—until a
      solution develops
    You get degraded results, waste your time and
      money, and you never establish professional
      proficiency.
Five steps to planning
        (and permit approval):
Establishing the boundaries of the field work
Locating sensitive sites and hazards
Determining how you will avoid or minimize
  effects to sensitive areas (i.e. establish
  protocols)
Instructing your working teams about how
   they‟ll implement the protocols
Monitoring in-the-field performance
  (somebody must be the “Coach”)
The Project begins. Money’s
 on the line. Somebody has to:
Find the landowners
Establish their correct tract boundaries (for
  permitting and ground control)
And you: must assume that all the
 information that you carefully collected is
 incorrect.
assume that all information is
  incorrect, regardless of source

All sources have incorrect data:
  • Tax assessors,
  • Land companies,
  • Digitized plats,
  • Other public and private domain data.
Field Support in Three Parts

1) Strategies to get you the best
   possible data

2) Logistical hoops to jump through
   ($), and

3) Tools that will help you get (and
   make...) correct information
Your Problem: Taxing agencies draw
 polygons to identify tracts, which is
 how they send tax bills…
 So, the shape and location of the
 tract doesn‟t really matter to them.
Your Solution: current aerial
 photography or satellite imagery,
 ortho-rectified to obvious, photo-
 identifiable ground control points.
Example:
  up-to-date satellite image vs. air
        photo vs. topo map
Satellite data have greater detail and
  geometric fidelity. They are only a
  few days old, and they‟re cheap.
Air photos are old, don‟t show recent
  construction activity, new structures
  or ponds.
Topo maps are even more out of date.
Satellite Data
Aerial Photography
Topographic maps
Red = Good
Yellow = Costing You Money
Accurate Cadastral Boundaries
   Corrected boundaries :
    • Prevents trespass
    • Builds confidence of landowners
    • Plan source and receiver offsets in “no
      permit” areas
    • Provides surveyors with correct
      mapping
    • Provides client with correct land
      mapping
Field Conditions
        that Explode Your Budget:
   Terrain & relief (slope)
   Soil type & erodeability
   Vegetation (i.e. what it is, what it will cost
    if damaged)
   Hydrologic features & drainage basins
   Weather
Arrange to get the right equipment in
  position in advance of need.
Knowing Slope & Surface Geology
Avoids This....Vibes can’t maintain coupling
          on steep, rocky slopes
Knowing hydrology will avoid running cables
    through drainages multiple times
Know your hydrology & soil types
so you can identify liquefaction areas
     (caused when vibes shake)
Know about new construction...without planning
  ahead, your sampling points will have to be
        dropped or offset “on the fly”.
How this will work
   Agenda:
    • Part 1: Case studies (natural disasters;
      environmental; damages & liabilities;
      exploration; logistical support)
    • Part 2: Photogeology; how images work
    • Part 3: Field work: it costs a lot.
      Getting better data; saving time and
      money on your surveys
    • Part 4: Other stuff to know, time
      permitting
Independent Explorationists:
   Lean operations, often rely on the work of
    consultants for photogeology.
   Many could be using remotely sensed
    data interactively.
   Work on hand is insufficient to support a
    remote sensing specialist of their own.
   Some are familiar with photogeology.
   One RSPg project can high-grade enough
    areas to support prospect-generation for
    two or three years.
Preparing for a Photogeology Study:
   Objectives: frontier, previewing, to buy
    leases or evaluate existing leases?
   What is the land type, topographic relief,
    jungle, arid....
   Best platform.
   Cost, budget, savings.
   Time of year.
   Scales.
   Using same data for logistics and
    documentation
The Future of Photogeology
   Image data is more accessible (in terms of speed
    and storage) with CDs, smaller computers,
    better software and training (more cross-
    pollenization with other disciplines).
   Small, special-purpose satellites are taking the
    place of large, multipurpose systems.
   There are no technological barriers to satellite
    data design or use; only markets are lacking.
   Precision Agriculture will drive the remote
    sensing market even more.
Important Issues for Remote Sensing
   Government space/business policy is
    unstable…short-term government budgetary
    processes make business‟ long-term planning
    needs treacherous.
   Government interests are long-term but business
    has short-term profit motives.
   Government/Industry partnerships are necessary
    if our nation is to stay competitive…other nations
    realize this critical need to cooperate and it is the
    U.S.'s critical shortcoming.
In Conclusion….
   Seismic and well logs, gravity and basement magnetics can
    confirm structures first detected photogeologically.
   Detecting rising hydrocarbons and hydrocarbon-induced
    chemical changes in soils can be done remotely and
    cheaply, especially as a lead tool.
   Select a contractor who speaks in terms you understand
    and impose the same standards you apply to other tools.
   The need to constrain Landsat interpretations with all
    available geologic data cannot be overemphasized.
   Remote sensing photogeology replaces no common tools;
    rather, it aids in the planning and layout of more expensive
    methods.
   Oil industry observers say “new technologies” will help
    today‟s explorationist survive in the face of rising costs and
    regulations. Few specify how, but it is clear that remote
    sensing photogeology can lower finding costs.
From Creekology to Rocket Science:
The Evolution of Remote Sensing/GIS
     in Oil and Gas Exploration
           A Presentation for

         2011 Texas GIS Forum
             October 26, 2011
              Austin, Texas

              David G. Koger

                Fort Worth
From Creekology to Rocket Science:
The Evolution of Remote Sensing/GIS
     in Oil and Gas Exploration
           A Presentation for

         2011 Texas GIS Forum
             October 26, 2011
              Austin, Texas

              David G. Koger

                Fort Worth

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From creekology to rocket science the evolution of remote sensing gis in oilgas exploration

  • 1. From Creekology to Rocket Science: The Evolution of Remote Sensing/GIS in Oil and Gas Exploration A Presentation for 2011 Texas GIS Forum October 26, 2011 Austin, Texas David G. Koger Fort Worth
  • 2. Becoming an Expert  takes 10,000 hours, timing & luck
  • 3. Becoming an Expert  takes 10,000 hours, timing & luck  and the desire to show up
  • 4. Becoming an Expert  takes 10,000 hours, timing & luck  the desire to show up  and learning “dialogues of business”
  • 5. Becoming an Expert  takes 10,000 hours, timing & luck  the desire to show up  and learning “dialogues of business”  and learning after school‟s out
  • 6. Becoming an Expert  takes 10,000 hours, timing & luck  the desire to show up  and learning “dialogues of business”  and learning after school‟s out  e.g. the expert mortician
  • 8. Creekology: Seeing into the Earth  „Seepology‟...Native Americans extracted medicinal goo  The first oil wildcatters drilled at the bends in streams  Early USGS maps showed rough stream drainage patterns
  • 9. Creekology  Satellite data—large scale and highly accurate—merged creekology with geology.  Photogeologic work was now possible without troublesome mosaicking.  Remotely sensed data are spatially and spectrally better than airphotos, and has  A greater variety of sun angles, moisture conditions, and seasonal samplings.
  • 10. How this will work  Agenda: • Part 1: Case studies (natural disasters; environmental; damages & liabilities; exploration; logistical support) • Part 2: Photogeology; how images work • Part 3: Field work: it costs a lot. Getting better data; saving time and money on your surveys • Part 4: Other stuff to know, time permitting
  • 11. Part 1: Case Studies ...Liabilities, Damages, Operations and Planning…
  • 12. Case study #1  Put it back the way you found it. (not an unreasonable request…)  What is a weed, after all? (everybody knows what a weed is, right?)  Causing damage to the bushes  and what‟s beneath the bushes (USLE).  Putting it back (how hard can that be?)
  • 13. Case study #1  Put it back the way you found it. (not an unreasonable request…)  What is a weed, after all? (everybody knows what a weed is, right?)  Causing damage to the bushes  and what‟s beneath the bushes (USLE).  Putting it back (how hard can that be?)
  • 14. Case study #1  Put it back the way you found it. (not an unreasonable request…)  What is a weed, after all? (everybody knows what a weed is, right?)  Causing damage to the bushes  and what‟s beneath the bushes (USLE).  Putting it back (how hard can that be?)
  • 15. Case study #1  Put it back the way you found it. (not an unreasonable request…)  What is a weed, after all? (everybody knows what a weed is, right?)  Causing damage to the bushes  and what‟s beneath the bushes (USLE).  Putting it back (how hard can that be?)
  • 16. Case study #1  Put it back the way you found it. (not an unreasonable request…)  What is a weed, after all? (everybody knows what a weed is, right?)  Causing damage to the bushes  and what‟s beneath the bushes (USLE).  Putting it back (how hard can that be?)
  • 17.
  • 18. Case study #2  300,000 acres burned up  Whose land was damaged?  What portions were grassland, crops, trees?  Where‟d the fire actually start?  Who‟s responsible?
  • 20. Wildfire 6 hrs later
  • 23. Fire Severity on Property Boundaries
  • 24. High Water Marks Creating up-to-date information. A word about coastlines, tides, erosion (and where the fish are).
  • 25.
  • 26.
  • 27. Freshwater or Ocean; currents and thermal differences for fishing
  • 28. Exploration Examples  Nebraska  Fayetteville Shale  Marcellus Shale  Romania  Paraguay  Costa Rica  Kansas DOE three times
  • 29. Exploration Examples  Nebraska  Fayetteville Shale  Marcellus Shale  Romania  Paraguay  Costa Rica  Kansas DOE three times
  • 30. Large-scale Data Management: Photogeology Mapping of Nebraska The goal was to foment exploration, so we conducted a photogeology study of Nebraska at medium scale, using satellite imagery, gravity and magnetics.
  • 31. Large-scale Data Management: Photogeology Mapping of Nebraska We acquired topographic maps at 1:250,000 and 1:100,000 scales) for spatial reference with the satellite imagery.
  • 32. Large-scale Data Management: Photogeology Mapping of Nebraska Structural interpretations were made from and overlaid onto the imagery.
  • 33. Large-scale Data Management: Photogeology Mapping of Nebraska The interpretations were overlaid onto topo maps to provide a universal map reference display.
  • 34. Large-scale Data Management: Photogeology Mapping of Nebraska A merge of imagery, map, and interpretation.
  • 35.
  • 36. Exploration Examples  Nebraska  Fayetteville Shale  Marcellus Shale  Romania  Paraguay  Costa Rica  Kansas DOE three times
  • 37. Landsat bands 7, 4, and 2; composited as color on the following slide
  • 40. Regional + Local (24K) Interpretations
  • 41.
  • 42.
  • 43.
  • 44. Exploration Examples  Nebraska  Fayetteville Shale  Marcellus Shale  Romania  Paraguay  Costa Rica  Kansas DOE three times
  • 45.
  • 46.
  • 47.
  • 48.
  • 49. Exploration Examples  Nebraska  Fayetteville Shale  Marcellus Shale  Romania  Paraguay  Costa Rica  Kansas DOE three times
  • 50. Romania  Identify features of exploration interest (e.g. fault/frax, structures, tonal anomalies)  Update WWII-era maps  Identify high-cost damage areas (e.g. vineyards....)
  • 51. Data Types & Sources: Multi-sensor merge (Landsat + SPOT) The area had only WWII-era maps....
  • 52. Data Types & Sources: Multi-sensor merge (Landsat + SPOT) This is the 5-meter panchromatic SPOT image that supplied the spatial detail in the study, while 28.5m Landsat data provided the spectral information.
  • 53. Data Types & Sources: Multi-sensor merge (Landsat + SPOT) The multi-band Landsat was encoded to hue and saturation, while the higher resolution SPOT was assigned to intensity.
  • 54. Data Types & Sources: Multisensor merge (Landsat + SPOT) The photogeology interpretations are overlaid.
  • 55. Data Types & Sources: Multisensor merge (Landsat + SPOT)
  • 56. Data Types & Sources: Multisensor merge (Landsat + SPOT)
  • 57. Exploration Examples  Nebraska  Fayetteville Shale  Marcellus Shale  Romania  Paraguay  Costa Rica  Kansas DOE three times
  • 58. Paraguay Information Needed Where are existing roads that can be used for moving equipment and laying out field work equipment, Where are the tracks of previous field work? Update maps...collect detailed knowledge of the area, Find water sources: rivers, ponds, springs.
  • 59. Gold = Your New, Geometrically Accurate Roadmap
  • 60. Exploration Examples  Nebraska  Fayetteville Shale  Marcellus Shale  Romania  Paraguay  Costa Rica  Kansas DOE three times
  • 64.
  • 65. Exploration Examples  Nebraska  Fayetteville Shale  Marcellus Shale  Romania  Paraguay  Costa Rica  Kansas DOE three times
  • 66. “Remote Sensing Image Analysis Toward Understanding Sequestration Potential of Southern Kansas” DE-FE0002056 – “Modeling CO2 Sequestration in Saline Aquifer and Depleted Oil Reservoir to Evaluate Regional CO2 Sequestration Potential of Ozark Plateau Aquifer System, South-Central Kansas” by David G. Koger Ralph N. Baker, PhD Fort Worth
  • 67. Information needed:  Is it safe to inject CO2?  Will it come back up?  How quickly?  Where?  Where might it get trapped?  What are the cost trade-offs?
  • 68. Remote Sensing to the Rescue • Help map the subsurface  Conduits / Compartments;  Migration fairways / Sealing mechanisms • Define structural & stratigraphic elements  these affect Fluid Movement
  • 69. (Information, continued) All of which supports: Environmental Risk Analysis and Helps determine reservoir suitability for CO2 storage
  • 70. Because knowing the contrasts of Conduits vs. Compartmentalization and Migration Pathways vs. Sealing Factors Must be understood & modeled to predict Fluid Movement and reservoir integrity because this is how we can know how and where groundwater flows and, therefore, How/if CO2 injections might affect the water table (e.g. we expect some CO2 leakage along fractures; high porosity/permeability zones are especially noteworthy….
  • 71. Regional Gravity & Magnetics  Define Major Basement Block Boundaries, Structural Grain
  • 72. Regional Gravity & Magnetics  Define Major Basement Block Boundaries, Structural Grain
  • 74. Local on top of Regional
  • 75.
  • 76.
  • 77.
  • 78. Exploration Examples  Nebraska  Fayetteville Shale  Marcellus Shale  Romania  Paraguay  Costa Rica  Kansas DOE three times
  • 79. “Remote Sensing Image Analysis of the Bemis-Schutts Field, Ellis County, Kansas” in support of U.S. Dept of Energy/KS Geological Survey’s DE-FE0004566 – “Prototyping and testing a new volumetric curvature tool for modeling reservoir compartments and leakage pathways in the Arbuckle saline aquifer: reducing uncertainty in CO2 storage and permanence” by David G. Koger Ralph N. Baker, PhD Koger Remote Sensing, Fort Worth
  • 84. How this will work  Agenda: • Part 1: Case studies (natural disasters; environmental; damages & liabilities; exploration; logistical support) • Part 2: Photogeology; how images work • Part 3: Field work: it costs a lot. Getting better data; saving time and money on your surveys • Part 4: Other stuff to know, time permitting
  • 85. How satellites work:  They collect their data with scanners. Other scanners are: • video cameras, • fax machines, • barcode readers, • Magnetic Resonance Imaging machines, • video game characters‟ vision...
  • 86. Part 2 (how images work)  About satellite data • How it collects & organizes data • Attributes of these data  Spectra, spatial, temporal  Photogeology for exploration
  • 87. Part 2 (how images work)  About satellite data • How data are collected & organized • Attributes of these data  Spectra, spatial, temporal  Photogeology for exploration
  • 88.
  • 90.
  • 91. Docks and Cranes pre-quake
  • 92. Docks and Cranes Collapsed in Water (after quake)
  • 96.
  • 97. Part 2 (how images work)  About satellite data • How it works • Attributes  Spectra, spatial, temporal  Photogeology for exploration
  • 98.
  • 100.
  • 101.
  • 102. Digital Image Processing “Pixel” = “picture element” ...one spatial unit plus the spectra.
  • 103. Part 2 (how images work)  About satellite data • How it works • Attributes  Spectra, spatial, temporal  Photogeology for exploration
  • 105. Reducing Data to Information A typical project area encompasses: •2-6 Landsat scenes (600MB to 1.8 GB raw data) •12-36 USGS raster topo sheets (500 Mb to 1.5 Gb) •Ancillary magnetics and gravity surveys (200 MB) •High resolution aerial imagery (800MB to 2 GB) For a total of 2.1 to 5 GB of raw data Color composites, PCAs, structural interpretations, and ancillary data can make 12-15 GB of additional files All this fuss over data selection, processing, and analysis is because the process must deliver the information needed to make decisions.
  • 106. Landsat TM processing Landsat Band 7 raw data with brightness and contrast stretches applied
  • 107. Landsat TM processing Same area: Band 1 raw data stretched
  • 108. Landsat TM processing Band 3-2-1 composite of raw data Same, stretched
  • 109. Landsat TM processing Band 7-5-4 composite of raw data Same, stretched
  • 110. Landsat TM processing Multitemporal Principal Components Analysis (or De-correlation Stretch).
  • 112. Part 2  About satellite data • How it works • Attributes  Spectra, spatial, temporal  Photogeology for exploration
  • 113. At left, March 12 shows vegetation patterns in the early spring (bright greens). At right, December 23 vegetation is dormant. Both images are “true.”
  • 114. Palo Pinto Landsat multi-temporal comparisons September and March
  • 115. Multi-temporal 1m data comparison for tax appraisal purposes
  • 116. Part 2  About satellite data • How it works • Attributes  Spectra, spatial, temporal  Photogeology for exploration
  • 117. You can never have too much information What you do have:  production trends,  a regional framework,  well logs here and there, and  maybe some field work.
  • 118. Available information is massive:  Surface and subsurface geology maps  Current and historic well logs  Topographic maps  Seismic analyses  Gravity surveys  Magnetic surveys  Satellite and aerial imagery  Geochem surveys
  • 119. The ideal tool would: 1) fill in every empty space of the mosaic 2) highlight anomalous conditions, and map structure: large folds and astroblemes or localized fracturing and reefs.
  • 120. An even better tool would: a) sample at intervals in time (all seasons, wet and drought conditions, over decades), and b) offer adaptive scale to support either frontier or mature basin analysis.
  • 121. Two Kinds of Tools: • Those that find structure • Those that find anomalous conditions Remote sensing does both
  • 122. The Crust of Earth is: • Thin, unstable, and floats • Bombarded with energy daily • Generates soil @ 3 tons per acre per year • Washed down and compacted daily
  • 123. Remote sensing photogeology is a blend of several disciplines:  optics  physics  electronics  cartography  natural science  computer sciences
  • 124. Patterns: Their causes and effects Subsurface activity imprints the surface for many reasons :  constant micro-earthquakes,  settling,  erosion,  micro-seepages.
  • 125. Microbes are everywhere!  We are 1/10 th us; 9/10th microbes.  H.pylori causes 90% of peptic ulcers.  Antibiotics fight harmful microbes.  Yogurt has good ones.  They‟re in amber, meteorites, Mars rocks, and 250 million-yr-old crystals.  A billion microbes in 1 gram of topsoil.  Dead microbes make topsoil.  Other microbes clean up oil spills.  A trillion are on each of your feet.
  • 126. Healthy topsoil…  retains water better,  resists erosion,  has more oxygen,  better nutrients,  Microbes and earthworms like it,  compacts less, and  is friendlier to roots.
  • 127. Hydrocarbon-eating microbes  Thrive above oil and gas reservoirs.  Create a magnetic residue.  Are counted.  Deplete oxygen in soil.  Do not build good soil.  Seeps are mostly vertical; dynamic. These conditions have been recorded for 39 years....
  • 130. The Information in Photogeology Lineaments: Faults, fractures, fracture orientation and joints can have surface expression as:  Linear escarpments. Changes in the directions they face can mean strike-slip faults.  Linear and right angle bends in drainage courses.  Drainages running in parallel.  Aligned drainages on opposing sides of a drainage divide.  Tributaries entering main streams in direct opposition.  Moisture accumulation in linear patterns; alignment of water bodies
  • 131. The Information in Photogeology Lineaments (continued):  Linear vegetation patterns due to water availability.  Aligned notches on ridge crests.  Subtle dip changes, varying lithologies or changes in rock texture.  Variation in thermal signature.  Large topographic trends align with basement lineaments.  High fracture densities enhance hydrocarbon mobility at depth
  • 132. The Information in Photogeology Positive Structures at Depth can appear as…  Surface tonal anomalies.  Circular features can indicate buried structure.  Vegetation differences: health, leaf water content, population distribution.  Differential compaction, loading, increased fracture density over and adjacent to buried structure.  Soil color and texture alterations…staining, bleaching, cobbling.  Local, slight topographic highs or lows.  Subtle variations in moisture accumulation on the flanks of buried structure.
  • 133. Mapping and GIS: making it all fit Google Earth: “cans” and “can’ts”: Very popular new web tool; •Fast and easy for finding places and routes •Reasonably accurate cartographic information; •High resolution imagery in some locations; •Excellent 3D visualization tool However: •Not accurate enough to be used as an exploration map •Image dates unknown •Most areas outside cities and large towns in low resolution •Color imagery not good enough for photogeologic analysis
  • 134. How this will work  Agenda: • Part 1: Case studies (natural disasters; environmental; damages & liabilities; exploration; logistical support) • Part 2: Photogeology; how images work • Part 3: Field work: it costs a lot. Getting better data; saving time and money on your surveys • Part 4: Other stuff to know, time permitting
  • 135. Field Work Support Requires Leadership… Knowing where you‟re going….
  • 136. Field Work Support in Three Parts 1) Strategies to get you the best possible data 2) Logistical hoops to jump through ($), and 3) Tools that will help you
  • 137. Wait a second: has your area been shot already? “Earth Detective” work on an unusual application for (free) satellite data....
  • 138. Has your area been shot?  Google Earth  Landsat 5  Landsat 7  Airphotos in archive • Military • DOT • USDA • Farm Service
  • 139. Has the area been shot?  The trouble with airphoto coverage: • it is spotty • often monochromatic • often mono-temporal  Satellite data • have an archive that goes back 29 years • they‟re inexpensive…mostly free • they cover 10,000 square miles • you get to choose:  the right sun angle  the right soil moisture  the right vegetation cover
  • 140. No shoots as of 29Jan95
  • 141. No shoots as of 21Oct05
  • 142. No shoots as of 30Oct08
  • 143. No shoots as of 29Nov09
  • 144. Has the area been shot?  The trouble with airphoto coverage: • it is spotty • often monochromatic • often mono-temporal  Satellite data • have an archive that goes back 29 years • they‟re inexpensive…mostly free • they cover 10,000 square miles • you get to choose:  the right sun angle  the right soil moisture  the right vegetation cover
  • 145. Yes, there were shoots in the area as of 18July06
  • 146. Only six months later, seeing it is difficult due to the low sun angle:
  • 147. What you should know about supporting field work  Somebody is responsible. Apparently, it‟s you.  Good information won‟t just happen…it demands good planning.  List all the things that can go wrong in the field. Plan for them.  Field work is expensive. Your project will go over budget unless good information supports your plan....  Collecting the best quality field data results from a good plan.
  • 148. Field work Support in Three Parts 1) Strategies to get you the best possible data 2) Logistical hoops to jump through ($), and 3) Tools that will help you
  • 149. The Subsurface ...is where the treasure—water or oil—is: how can we see down there?
  • 150. On the Geology Side: Expensive subsurface surveys are useless unless they produce a proper image of the subsurface. Advanced modeling—before the shoot design—of the strata below will dictate your: • receiver and source spacing, • the location and spacing of lines • the geometric organization of the signal source and receiver locations, i.e. the design.
  • 154. Satellite data on DEM: slippery slopes
  • 155. Surface composition: i.e. slippery soils
  • 156. The Subsurface in 3-D  Generate a model of the earth at depth using: • surface & subsurface structure maps, • velocity information, and • other seismic data.  Ray tracing from the target horizons will identify your optimum shoot parameters
  • 158. Initial Design  Test it to ensure that subsurface coverage is not compromised.  A full patch, 3D ray tracing shows: • which parameters will best image your target.  3-D ray tracing may be re-run after “no permit areas” or other obstacles are found.
  • 160. Final Design  Subsurface model is in place  Offset sources & receivers have been ray traced in the model  Hazards are identified  Protocol for handling offsets is established  …meaning: geophysical decisions are not left to the field crew  We‟re now ready to go to the field
  • 161. Field Support in Three Parts 1) Strategies to get you the best possible data 2) Logistical hoops to jump through ($), and 3) Tools that will help you
  • 162. Knowing What’s in Real World… Dealing with it.
  • 163. Realities of Designing Field Work  The goals of field work and land owners are often in conflict.  It takes knowledge, effort, and time, to: • identify the project‟s requirements and • endure the permitting process.  A third party consultant will save you time and money.
  • 164. Two Costly Philosophies  Being Rigorous: • a strict technical design w/o regard for obstacles on the ground… Your field personnel have to deal with whatever obstacles they encounter.  Being Serendipitous: • personnel are sent to the field w/no coordination... They wander around—on your dime—until a solution develops You get degraded results, waste your time and money, and you never establish professional proficiency.
  • 165. Five steps to planning (and permit approval): Establishing the boundaries of the field work Locating sensitive sites and hazards Determining how you will avoid or minimize effects to sensitive areas (i.e. establish protocols) Instructing your working teams about how they‟ll implement the protocols Monitoring in-the-field performance (somebody must be the “Coach”)
  • 166. The Project begins. Money’s on the line. Somebody has to: Find the landowners Establish their correct tract boundaries (for permitting and ground control) And you: must assume that all the information that you carefully collected is incorrect.
  • 167. assume that all information is incorrect, regardless of source All sources have incorrect data: • Tax assessors, • Land companies, • Digitized plats, • Other public and private domain data.
  • 168. Field Support in Three Parts 1) Strategies to get you the best possible data 2) Logistical hoops to jump through ($), and 3) Tools that will help you get (and make...) correct information
  • 169. Your Problem: Taxing agencies draw polygons to identify tracts, which is how they send tax bills… So, the shape and location of the tract doesn‟t really matter to them. Your Solution: current aerial photography or satellite imagery, ortho-rectified to obvious, photo- identifiable ground control points.
  • 170. Example: up-to-date satellite image vs. air photo vs. topo map Satellite data have greater detail and geometric fidelity. They are only a few days old, and they‟re cheap. Air photos are old, don‟t show recent construction activity, new structures or ponds. Topo maps are even more out of date.
  • 174. Red = Good Yellow = Costing You Money
  • 175. Accurate Cadastral Boundaries  Corrected boundaries : • Prevents trespass • Builds confidence of landowners • Plan source and receiver offsets in “no permit” areas • Provides surveyors with correct mapping • Provides client with correct land mapping
  • 176.
  • 177. Field Conditions that Explode Your Budget:  Terrain & relief (slope)  Soil type & erodeability  Vegetation (i.e. what it is, what it will cost if damaged)  Hydrologic features & drainage basins  Weather Arrange to get the right equipment in position in advance of need.
  • 178. Knowing Slope & Surface Geology Avoids This....Vibes can’t maintain coupling on steep, rocky slopes
  • 179. Knowing hydrology will avoid running cables through drainages multiple times
  • 180. Know your hydrology & soil types so you can identify liquefaction areas (caused when vibes shake)
  • 181. Know about new construction...without planning ahead, your sampling points will have to be dropped or offset “on the fly”.
  • 182.
  • 183.
  • 184.
  • 185.
  • 186. How this will work  Agenda: • Part 1: Case studies (natural disasters; environmental; damages & liabilities; exploration; logistical support) • Part 2: Photogeology; how images work • Part 3: Field work: it costs a lot. Getting better data; saving time and money on your surveys • Part 4: Other stuff to know, time permitting
  • 187. Independent Explorationists:  Lean operations, often rely on the work of consultants for photogeology.  Many could be using remotely sensed data interactively.  Work on hand is insufficient to support a remote sensing specialist of their own.  Some are familiar with photogeology.  One RSPg project can high-grade enough areas to support prospect-generation for two or three years.
  • 188. Preparing for a Photogeology Study:  Objectives: frontier, previewing, to buy leases or evaluate existing leases?  What is the land type, topographic relief, jungle, arid....  Best platform.  Cost, budget, savings.  Time of year.  Scales.  Using same data for logistics and documentation
  • 189. The Future of Photogeology  Image data is more accessible (in terms of speed and storage) with CDs, smaller computers, better software and training (more cross- pollenization with other disciplines).  Small, special-purpose satellites are taking the place of large, multipurpose systems.  There are no technological barriers to satellite data design or use; only markets are lacking.  Precision Agriculture will drive the remote sensing market even more.
  • 190. Important Issues for Remote Sensing  Government space/business policy is unstable…short-term government budgetary processes make business‟ long-term planning needs treacherous.  Government interests are long-term but business has short-term profit motives.  Government/Industry partnerships are necessary if our nation is to stay competitive…other nations realize this critical need to cooperate and it is the U.S.'s critical shortcoming.
  • 191. In Conclusion….  Seismic and well logs, gravity and basement magnetics can confirm structures first detected photogeologically.  Detecting rising hydrocarbons and hydrocarbon-induced chemical changes in soils can be done remotely and cheaply, especially as a lead tool.  Select a contractor who speaks in terms you understand and impose the same standards you apply to other tools.  The need to constrain Landsat interpretations with all available geologic data cannot be overemphasized.  Remote sensing photogeology replaces no common tools; rather, it aids in the planning and layout of more expensive methods.  Oil industry observers say “new technologies” will help today‟s explorationist survive in the face of rising costs and regulations. Few specify how, but it is clear that remote sensing photogeology can lower finding costs.
  • 192. From Creekology to Rocket Science: The Evolution of Remote Sensing/GIS in Oil and Gas Exploration A Presentation for 2011 Texas GIS Forum October 26, 2011 Austin, Texas David G. Koger Fort Worth
  • 193. From Creekology to Rocket Science: The Evolution of Remote Sensing/GIS in Oil and Gas Exploration A Presentation for 2011 Texas GIS Forum October 26, 2011 Austin, Texas David G. Koger Fort Worth