Difference between revisions of "Impact crater"

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==Compute probability of a crater==
 
==Compute probability of a crater==
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Stewart (1999)<ref>Stewart, S (1999), Seismic interpretation of circular geological structures, Petroleum Geoscience 5, 273–285.</ref> gave some equations from Hughes 1998<ref>Hughes, D, 1998, The mass distribution of the crater-producing bodies. In ''Meteorites: Flux with time and impact effects'', Geological Society of London Special Publication 140, 31–42. </ref> and Davis 1986<ref>Davis, J, 1986, ''Statistics and data analysis in geology'', John Wiley & Sons, New York.</ref>. The probability ''P'' of encountering ''r'' craters of diameter 1 &le;''d'' &le; 500 or more in an area ''A'' over a time period ''t'' years is given by
 
Stewart (1999)<ref>Stewart, S (1999), Seismic interpretation of circular geological structures, Petroleum Geoscience 5, 273–285.</ref> gave some equations from Hughes 1998<ref>Hughes, D, 1998, The mass distribution of the crater-producing bodies. In ''Meteorites: Flux with time and impact effects'', Geological Society of London Special Publication 140, 31–42. </ref> and Davis 1986<ref>Davis, J, 1986, ''Statistics and data analysis in geology'', John Wiley & Sons, New York.</ref>. The probability ''P'' of encountering ''r'' craters of diameter 1 &le;''d'' &le; 500 or more in an area ''A'' over a time period ''t'' years is given by
  

Revision as of 17:52, 5 August 2019

Impact craters are a rare type of circular feature in seismic data. If you find a round thing in your seismic, it might help to know what the probability of it being an impact structure is.

The Steen River crater in northern Alberta is a Cretaceous-age impact buried in the subsurface; there are hydrocarbons associated with the feature.

Compute probability of a crater

Stewart (1999)[1] gave some equations from Hughes 1998[2] and Davis 1986[3]. The probability P of encountering r craters of diameter 1 ≤d ≤ 500 or more in an area A over a time period t years is given by

where

and

These equations are built into the Wolfram Alpha Widget at right (requires JavaScript). You will probably want to leave the number of craters at 1; enter the size of structure you are concerned with — perhaps you have observed a circular feature in a seismic reflection survey; give the area of interest, and the time period. Take note of the caveats, given below.

Example

The probability of an impact structure 1 km or greater in diameter in an Albertan township (36 square miles = 93 km2) in the Cenozoic (65 Ma) is 0.012.

Caveats

The default diameter is rather small: the minimum size required to reach the ground intact is estimated to be 100–200 m diameter, resulting in a crater 2–3 km in diameter (Chapman & Morrison 1994[4]). Bolides can break up, however, resulting in smaller craters.

Clearly, you need to think a bit about depositional environments and periods of uplift and erosion. Deep marine environments don't record small structures. Mountains won't result in a nice crater except for large bolides. When you consider erosion, it helps to know that, while the initial (transient) crater may have a depth/diameter ratio of 0.3, a typical final ratio is 0.1.

Also, note that estimates of terrestrial impact flux λ vary by at least a factor of two.

References

  1. Stewart, S (1999), Seismic interpretation of circular geological structures, Petroleum Geoscience 5, 273–285.
  2. Hughes, D, 1998, The mass distribution of the crater-producing bodies. In Meteorites: Flux with time and impact effects, Geological Society of London Special Publication 140, 31–42.
  3. Davis, J, 1986, Statistics and data analysis in geology, John Wiley & Sons, New York.
  4. Chapman & Morrison 1994, Impacts on the Earth by asteroids and comets: assessing the hazard. Nature 367, 33–40.