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Geologic Resources and Earth’s Systems
• Geologic resources - valuable materials of geologic origin that
can be extracted from the Earth
– Many geologic resources originate in the hydrosphere
• Petroleum and coal come from organisms that lived and died in water
• Halite (salt) and other evaporite minerals come from dry lake beds
– Weathering interactions between geosphere, atmosphere and
hydrosphere produce metal oxide ores
– Humans (biosphere) interact directly with the geosphere, hydrosphere,
and atmosphere when extracting and utilizing geologic resources
– Groundwater (hydrosphere) is a renewable geologic resource
• If it can’t be grown, it must be mined
Types of Geologic Resources
• Geologic resources are grouped into three
major categories:
– Energy resources - petroleum (oil and
natural gas), coal, uranium, geothermal
resources
– Metals - iron, copper, aluminum, lead, zinc,
gold, silver, platinum
– Non-metallic resources - sand and gravel,
limestone, building stone, salt, sulfur, gems,
gypsum, phosphates, groundwater, etc.
Resources and Reserves
• Resources - the total amount of a
valuable geologic material in all
deposits, discovered and
undiscovered
• Reserves - discovered deposits of
geologic resources that can be
extracted economically and legally
under present conditions
– The short-term supply of a geologic
materials
Energy Resources - Coal
• Fossil fuels (oil, natural gas,
and coal) account for nearly
90% of U.S. energy
• Coal is a sedimentary rock that
forms from the compaction of
plant material that has not
completely decayed
– Forms from shallow burial and
compaction of peat
• Four varieties of coal
– Lignite (brown coal) is soft and crumbly
– Sub-bituminous and bituminous coal (soft coal)
• black and dusty
• burn with a smoky flame
• commonly strip-mined
– Anthracite (hard coal)
• shiny and dust-free
• burns with a smokeless flame
• low-level metamorphic rock
• Burning of high-sulfur coal can produce acid rain;
strip mines can scar landscape
• U.S. coal reserves could last for centuries
Energy Resources - Coal
Energy Resources
-Petroleum
• Petroleum - oil and natural gas
- occurs in underground pools
• Occurrence of oil pools requires:
– A source rock (rich in organic matter)
– A reservoir rock in which it can be
stored and transmitted (e.g., sandstone)
– An oil trap (set of conditions holding
rock in reservoir rock and preventing
migration)
– Deep enough burial (and sufficient
time) to “cook” the oil and gas out of
the organic matter
Structural Traps
for Gas and Oil
2300 m – 4600 m = Oil formation
4600+ m = Gas formation
Eroded anticline forms trap in Landers oil field in Wyoming.
Energy Resources - Petroleum
Other Oil Traps in Geological Structures
Petroleum Recovery
• Oil fields are regions underlain by
one or more oil pools
– Largest in U.S. are in Texas and Alaska
• Oil and natural gas are removed through
wells drilled down into an oil trap within
a reservoir rock
• Negative environmental effects resulting
from oil recovery and transport include oil
spills, brine contamination of surface
water, and ground subsidence
Oil Peak, Oil Panic ?
(Study by Amos Nur - Stanford)
U.S., Canada, Japan, Germany, France, Italy, UK, are the biggest
consumers of oil reserves worldwide.
Oil Peaks – 1960's
In the 1850's oil mainly used
for kerosene lamps – remaining
was burned or disgarded.
Current oil production rates peaked
in 1960's but U.S. consumption rates
increase dramatically above this.
Don't panic!
-Try to conserve energy
-Seek alternative energy sources
At current rate of use, worldwide oil reserves should last 30-40 years,
and natural gas reserves somewhat longer (estimates from USGS)
Petroleum Reserves
Petroleum Reserves
• As petroleum prices rise, alternate petroleum
sources, such as heavy crude, oil shale and
oil sand, will be increasingly exploited
– Heavy crude is dense, viscous petroleum
– Oil shale is black or brown shale with high solid
organic matter content from which oil can be
extracted by distillation
– Oil sands (or tar sands) are asphalt-cemented sand
or sandstone deposits
Jobs and Salaries in Geology
Starting salaries for petroleum geologists with 0-2 yrs experience.
Mixture of B.S. and M.S. Degrees.
Jobs and Salaries in Geology
Geologists in Environmental (e.g. EPA, Geotechnical firms) and
Geologists in Government make $ 50 K – 75 K
Geology Ph.D. faculty starting salaries in 2007 ($70 K – 80 K)
Metals and Ores
• Metal ores - naturally occurring materials that can
be profitably mined
• Whether or not a mineral deposit is an ore
depends on chemical composition, the percent
extractable metal, and current market value of the
metal
• Metallic ore deposits originate from crystal
settling in igneous intrusions, hydrothermal fluids
cooling in pores and factures, chemical
precipitation in water, or sedimentation in
rivers (placers)
Mining and Metals
• Mining can be done at Earth’s surface
(strip mines, open-pit mines, and placer
mines) or underground
– Metals mined include iron, copper,
aluminum, lead, zinc, silver, gold and many
others
• With care, negative environmental
effects of mining, including unsightly
tailings piles, surface scars, land
subsidence, and acid mine drainage can
be minimized
Non-metallic Resources
• Non-metallic resources - not mined to extract a
metal or an energy source
– construction materials
• sand, gravel, limestone, and gypsum
– agriculture
• phosphate, nitrate and potassium compounds)
– industrial uses
• rock salt, sulfur, asbestos)
– gemstones
• diamonds, rubies, etc.
– household and business products
• glass sand, fluorite, diatomite, graphite)

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Traps in Petroleum exploration

  • 1. Geologic Resources and Earth’s Systems • Geologic resources - valuable materials of geologic origin that can be extracted from the Earth – Many geologic resources originate in the hydrosphere • Petroleum and coal come from organisms that lived and died in water • Halite (salt) and other evaporite minerals come from dry lake beds – Weathering interactions between geosphere, atmosphere and hydrosphere produce metal oxide ores – Humans (biosphere) interact directly with the geosphere, hydrosphere, and atmosphere when extracting and utilizing geologic resources – Groundwater (hydrosphere) is a renewable geologic resource • If it can’t be grown, it must be mined
  • 2. Types of Geologic Resources • Geologic resources are grouped into three major categories: – Energy resources - petroleum (oil and natural gas), coal, uranium, geothermal resources – Metals - iron, copper, aluminum, lead, zinc, gold, silver, platinum – Non-metallic resources - sand and gravel, limestone, building stone, salt, sulfur, gems, gypsum, phosphates, groundwater, etc.
  • 3. Resources and Reserves • Resources - the total amount of a valuable geologic material in all deposits, discovered and undiscovered • Reserves - discovered deposits of geologic resources that can be extracted economically and legally under present conditions – The short-term supply of a geologic materials
  • 4. Energy Resources - Coal • Fossil fuels (oil, natural gas, and coal) account for nearly 90% of U.S. energy • Coal is a sedimentary rock that forms from the compaction of plant material that has not completely decayed – Forms from shallow burial and compaction of peat
  • 5. • Four varieties of coal – Lignite (brown coal) is soft and crumbly – Sub-bituminous and bituminous coal (soft coal) • black and dusty • burn with a smoky flame • commonly strip-mined – Anthracite (hard coal) • shiny and dust-free • burns with a smokeless flame • low-level metamorphic rock • Burning of high-sulfur coal can produce acid rain; strip mines can scar landscape • U.S. coal reserves could last for centuries Energy Resources - Coal
  • 6. Energy Resources -Petroleum • Petroleum - oil and natural gas - occurs in underground pools • Occurrence of oil pools requires: – A source rock (rich in organic matter) – A reservoir rock in which it can be stored and transmitted (e.g., sandstone) – An oil trap (set of conditions holding rock in reservoir rock and preventing migration) – Deep enough burial (and sufficient time) to “cook” the oil and gas out of the organic matter
  • 7. Structural Traps for Gas and Oil 2300 m – 4600 m = Oil formation 4600+ m = Gas formation
  • 8. Eroded anticline forms trap in Landers oil field in Wyoming. Energy Resources - Petroleum
  • 9. Other Oil Traps in Geological Structures
  • 10. Petroleum Recovery • Oil fields are regions underlain by one or more oil pools – Largest in U.S. are in Texas and Alaska • Oil and natural gas are removed through wells drilled down into an oil trap within a reservoir rock • Negative environmental effects resulting from oil recovery and transport include oil spills, brine contamination of surface water, and ground subsidence
  • 11. Oil Peak, Oil Panic ? (Study by Amos Nur - Stanford) U.S., Canada, Japan, Germany, France, Italy, UK, are the biggest consumers of oil reserves worldwide.
  • 12. Oil Peaks – 1960's In the 1850's oil mainly used for kerosene lamps – remaining was burned or disgarded. Current oil production rates peaked in 1960's but U.S. consumption rates increase dramatically above this. Don't panic! -Try to conserve energy -Seek alternative energy sources
  • 13. At current rate of use, worldwide oil reserves should last 30-40 years, and natural gas reserves somewhat longer (estimates from USGS) Petroleum Reserves
  • 14. Petroleum Reserves • As petroleum prices rise, alternate petroleum sources, such as heavy crude, oil shale and oil sand, will be increasingly exploited – Heavy crude is dense, viscous petroleum – Oil shale is black or brown shale with high solid organic matter content from which oil can be extracted by distillation – Oil sands (or tar sands) are asphalt-cemented sand or sandstone deposits
  • 15. Jobs and Salaries in Geology Starting salaries for petroleum geologists with 0-2 yrs experience. Mixture of B.S. and M.S. Degrees.
  • 16. Jobs and Salaries in Geology Geologists in Environmental (e.g. EPA, Geotechnical firms) and Geologists in Government make $ 50 K – 75 K Geology Ph.D. faculty starting salaries in 2007 ($70 K – 80 K)
  • 17. Metals and Ores • Metal ores - naturally occurring materials that can be profitably mined • Whether or not a mineral deposit is an ore depends on chemical composition, the percent extractable metal, and current market value of the metal • Metallic ore deposits originate from crystal settling in igneous intrusions, hydrothermal fluids cooling in pores and factures, chemical precipitation in water, or sedimentation in rivers (placers)
  • 18. Mining and Metals • Mining can be done at Earth’s surface (strip mines, open-pit mines, and placer mines) or underground – Metals mined include iron, copper, aluminum, lead, zinc, silver, gold and many others • With care, negative environmental effects of mining, including unsightly tailings piles, surface scars, land subsidence, and acid mine drainage can be minimized
  • 19. Non-metallic Resources • Non-metallic resources - not mined to extract a metal or an energy source – construction materials • sand, gravel, limestone, and gypsum – agriculture • phosphate, nitrate and potassium compounds) – industrial uses • rock salt, sulfur, asbestos) – gemstones • diamonds, rubies, etc. – household and business products • glass sand, fluorite, diatomite, graphite)