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Mantle 3 He and CO 2 degassing in carbonic and geothermal springs of Colorado and implications for neotectonics of the Rocky Mountains Karl E. Karlstrom, Laura J. Crossey, David R. Hilton, and Peter H. Barry
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Mantle 3 He and CO 2 degassing in carbonic and geothermal springs of Colorado and implications for neotectonics of the Rocky Mountains Karl E. Karlstrom,

Jan 02, 2016

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Page 1: Mantle 3 He and CO 2 degassing in carbonic and geothermal springs of Colorado and implications for neotectonics of the Rocky Mountains Karl E. Karlstrom,

Mantle 3He and CO2 degassing in carbonic and geothermal springs of Colorado and implications for neotectonics of the Rocky Mountains

Karl E. Karlstrom, Laura J. Crossey, David R. Hilton, and Peter H. Barry

Page 2: Mantle 3 He and CO 2 degassing in carbonic and geothermal springs of Colorado and implications for neotectonics of the Rocky Mountains Karl E. Karlstrom,

Introduction• What is the topic of this paper? What are they saying that is new?

Page 3: Mantle 3 He and CO 2 degassing in carbonic and geothermal springs of Colorado and implications for neotectonics of the Rocky Mountains Karl E. Karlstrom,

Introduction• What is the topic of this paper? What are they saying that is new?

“This paper shows that hot springs, carbonic springs, and CO2 regional gas fields can be surface vent regions for degassing of mantle volatiles in continental regions that are undergoing lithospheric extension and epeirogenic uplift.”

Page 4: Mantle 3 He and CO 2 degassing in carbonic and geothermal springs of Colorado and implications for neotectonics of the Rocky Mountains Karl E. Karlstrom,

Helium-3 vs Helium-4• Helium-3 is a primordial substance in the

Earth's mantle, considered to have become entrapped within the Earth during planetary formation.

Page 5: Mantle 3 He and CO 2 degassing in carbonic and geothermal springs of Colorado and implications for neotectonics of the Rocky Mountains Karl E. Karlstrom,

Helium-3 vs Helium-4• Helium-3 is a primordial substance in the

Earth's mantle, considered to have become entrapped within the Earth during planetary formation.

• Helium-4 is by far the most abundant of the two naturally occurring isotopes of helium, making up about 99.99986% of the helium on Earth

Page 6: Mantle 3 He and CO 2 degassing in carbonic and geothermal springs of Colorado and implications for neotectonics of the Rocky Mountains Karl E. Karlstrom,

Figure 1• What information

is the data attempting to convey?

Page 7: Mantle 3 He and CO 2 degassing in carbonic and geothermal springs of Colorado and implications for neotectonics of the Rocky Mountains Karl E. Karlstrom,

Figure 1• What information

is the data attempting to convey?

• What is Rc/Ra?

Page 8: Mantle 3 He and CO 2 degassing in carbonic and geothermal springs of Colorado and implications for neotectonics of the Rocky Mountains Karl E. Karlstrom,

Figure 1• What information

is the data attempting to convey?

• What is Rc/Ra?

• What does “Air Corrected” mean?

Page 9: Mantle 3 He and CO 2 degassing in carbonic and geothermal springs of Colorado and implications for neotectonics of the Rocky Mountains Karl E. Karlstrom,

Figure 1• What information

is the data attempting to convey?

• What is Rc/Ra?

• What does “Air Corrected” mean?

• How do we measure helium ratios?

Page 10: Mantle 3 He and CO 2 degassing in carbonic and geothermal springs of Colorado and implications for neotectonics of the Rocky Mountains Karl E. Karlstrom,

Figure 2• What is this plot

trying to say?

Page 11: Mantle 3 He and CO 2 degassing in carbonic and geothermal springs of Colorado and implications for neotectonics of the Rocky Mountains Karl E. Karlstrom,

Modeling Sources of CO2

Sources that contribute to the CO2 load of springs include: (1) dissolution of carbonates (Ccarb), for example from Paleozoic carbonates along flow paths; (2) carbon of organic origin (Corg), including soil gas; and (3) deeply sourced (endogenic) CO2 (Cendo).

• What method is used to derive from which source the CO2 came from?

Page 12: Mantle 3 He and CO 2 degassing in carbonic and geothermal springs of Colorado and implications for neotectonics of the Rocky Mountains Karl E. Karlstrom,

Figure 3

Page 13: Mantle 3 He and CO 2 degassing in carbonic and geothermal springs of Colorado and implications for neotectonics of the Rocky Mountains Karl E. Karlstrom,

Figure 4• What are the

trends being illustrated?

Page 14: Mantle 3 He and CO 2 degassing in carbonic and geothermal springs of Colorado and implications for neotectonics of the Rocky Mountains Karl E. Karlstrom,

CO2 Flux through Springs

• 109 moles/yr =44 million kg per year• Almost the weight of the Titanic, per year

Page 15: Mantle 3 He and CO 2 degassing in carbonic and geothermal springs of Colorado and implications for neotectonics of the Rocky Mountains Karl E. Karlstrom,

CO2 Flux through Springs

• 109 moles/yr =44 million kg per year• Almost the weight of the Titanic, per year!

• 1011 moles/year • Amount of mass converted to energy by the sun in 1 sec.

Page 16: Mantle 3 He and CO 2 degassing in carbonic and geothermal springs of Colorado and implications for neotectonics of the Rocky Mountains Karl E. Karlstrom,

CO2 Flux through Springs

• 109 moles/yr =44 million kg per year• Almost the weight of the Titanic, per year!

• 1011 moles/year • ~ amount of mass converted to energy by the sun in 1 sec.

• 1012 moles/year• ~10 X the mass of all humans alive!

Page 17: Mantle 3 He and CO 2 degassing in carbonic and geothermal springs of Colorado and implications for neotectonics of the Rocky Mountains Karl E. Karlstrom,

Conclusions• Anything else?