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Page 1: A Paleogeographic Reconstruction of Impact Craters

A Paleogeographic Reconstruction A Paleogeographic Reconstruction of Impact Cratersof Impact Craters

April 19, 2008April 19, 2008

Catherine JuranekCatherine Juranek

Dr. David M. BestDr. David M. Best

Page 2: A Paleogeographic Reconstruction of Impact Craters

Earth’s GeologyEarth’s Geology

4.6 billion years old4.6 billion years old

Plate tectonic movementPlate tectonic movement– Arizona has moved through 65° latitude in Arizona has moved through 65° latitude in

past 500 million years [20°S to 45°N] past 500 million years [20°S to 45°N]

174 extraterrestrial impacts174 extraterrestrial impacts

Photo courtesy of: Dr. Ron Blakey, NAU

Page 3: A Paleogeographic Reconstruction of Impact Craters

South America & AfricaSouth America & Africa

19 impactsDensity: 1/614K mi2

8 impactsDensity: 1/861K mi2

Photos courtesy of: The Planetary and Space Science CentreUniversity of New BrunswickFredericton, New Brunswick, Canada

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Asia & Australia

Photos courtesy of: The Planetary and Space Science CentreUniversity of New BrunswickFredericton, New Brunswick, Canada

27 impactsDensity: 1/635K mi2

26 impactsDensity: 1/114K mi2

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North America & EuropeNorth America & Europe

57 impactsDensity: 1/167K mi2

Photos courtesy of: The Planetary and Space Science CentreUniversity of New BrunswickFredericton, New Brunswick, Canada

37 impactsDensity: 1/108K mi2

Page 6: A Paleogeographic Reconstruction of Impact Craters

Paleomapping SoftwarePaleomapping Software

PointTrackerPointTracker– Plots current impact positions in terms of Plots current impact positions in terms of

paleolocations in past geologic timepaleolocations in past geologic time

PlateTrackerPlateTracker– Moves plates back in geologic time to focus Moves plates back in geologic time to focus

PointTracker locationsPointTracker locations

ARCGISARCGIS– Mapping toolMapping tool

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ResultsResults

No correlationNo correlation

Impact Crater Analysisy = 0.0743x + 5.4407

R2 = 0.0094

-90

-60

-30

0

30

60

90

0 50 100 150 200

Diameter (km)

La

titu

de

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ResultsResults

Youngest/oldest correlationYoungest/oldest correlation

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ResultsResults

26 of 31 youngest are the smallest26 of 31 youngest are the smallest

Impact Crater Analysis of Sizey = 13.542x + 18.796

R2 = 0.2

05

10152025303540

0 0.5 1 1.5 2 2.5 3 3.5 4

Age (Ma)

Dia

met

er (k

m)

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ResultsResults

Unprocessed data pointsUnprocessed data points– 33 craters < 10 million years old33 craters < 10 million years old– 13 craters > 600 million years old13 craters > 600 million years old

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ResultsResults

Correlation: Younger – northCorrelation: Younger – north

Older - southOlder - south

Impact Crater Analysis

y = -0.0112x + 15.333

R2 = 0.015

-90

-60

-30

0

30

60

90

10 110 210 310 410 510 610

Age (Ma)

La

titu

de

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ConclusionsConclusions

26 of 30 youngest craters are the smallest26 of 30 youngest craters are the smallest– Ancient Earth atmospheric effectAncient Earth atmospheric effect– Size of extraterrestrial bodies over timeSize of extraterrestrial bodies over time– Erosion of older smaller cratersErosion of older smaller craters

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ConclusionsConclusions

Correlation between latitude and ageCorrelation between latitude and age

Division at 310 million yearsDivision at 310 million years62% older craters in southern latitudes and 62% older craters in southern latitudes and 85% younger craters in northern latitudes85% younger craters in northern latitudes

Possible explanation: shift of land massesPossible explanation: shift of land masses

Does not explain latitudinal differences in Does not explain latitudinal differences in

South America and AfricaSouth America and Africa

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ChallengesChallenges

No record of oceanic impactsNo record of oceanic impacts

Software restrictionsSoftware restrictions– Posit processing limited to 10-600 my onlyPosit processing limited to 10-600 my only– Posits 10-100 myo rounded to nearest 10 myPosits 10-100 myo rounded to nearest 10 my– Posits 100-600 myo rounded to nearest 20 myPosits 100-600 myo rounded to nearest 20 my

Graphing and mapping optionsGraphing and mapping options

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What’s in the Future?What’s in the Future?

Further AnalysisFurther Analysis

Comparison with terrestrial/marine boundariesComparison with terrestrial/marine boundaries

Spatial analysis of impacts Spatial analysis of impacts

Using nearest neighbor statisticsUsing nearest neighbor statistics

Determine random vs clustered patternsDetermine random vs clustered patterns

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Africa and South America – The FITAfrica and South America – The FIT

Photos courtesy of: The Planetary and Space Science CentreUniversity of New BrunswickFredericton, New Brunswick, Canada

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What’s in the Future?What’s in the Future?

Possible ConnectionsPossible Connections

Theory of antipodal focusingTheory of antipodal focusing

Astronomical implicationsAstronomical implications

Evidence of asteroid stormsEvidence of asteroid storms

Asteroids impacts as further proof of plate tectonicsAsteroids impacts as further proof of plate tectonics

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QuestionsQuestions

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