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Published byRobert Walsingham Modified over 9 years ago
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Optical Stratigraphy of a Wasatch fault trench wall and a Maritian surface using watershed-based segmentation Chaiwoot Boonyasiriwat Julie Willis Jerry Schuster Chris Duross
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Motivation for digital trench wall logging Algorithm for separating rocks from fill Statistics Mars
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Pre-earthquake Earthquake 900 years later Development of a colluvial wedge Motivation for digital trench wall logging
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Mapleton, Utah “mega-trench”
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1 meter Develop a rock segmentation algorithm to separate clasts from matrix. Determine whether colluvial wedges, debris flows and channel deposits can be statistically differentiated. Mapleton Trench Level 1 1 m 1 meter Colluvial Wedge Debris Flow Channel Deposit
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10 cm
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Channel Deposit 2
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1 meter Algorithm successfully separates rocks from fill – 80% accuracy. Can colluvial wedges, debris flows and channel deposits be statistically differentiated? Compare: Orientation, Eccentricity, Percent Rock Mapleton Trench Level 1 1 m Colluvial Wedge Debris Flow Channel Deposit
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Colluvial Wedge 1 Orientation? Eccentricity? Percent Rock?
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Colluvial Wedge 3 Orientation? Eccentricity? Percent Rock?
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Debris Flow 1 Orientation? Eccentricity? Percent Rock?
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Channel Deposit 1 Orientation? Eccentricity? Percent Rock?
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Eccentricity 2.8% < 0.2 12.5% < 0.2 2.5% < 0.2 Percent Rock Channel Deposits: 32 % Colluvial Wedge: 48 % Debris Flow: 42 %
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Clast Orientation
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1 meter Can colluvial wedges, debris flows and channel deposits be statistically differentiated? Orientation – Colluvial Wedge Eccentricity, Percent Rock – Channel Deposits Mapleton Trench Level 1 1 m Colluvial Wedge Debris Flow Channel Deposit
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1 meter Future work: Use the segmentation algorithm to objectively log trench walls and build data for more rigorous statistics Mars and beyond... Mapleton Trench Level 1 1 m Colluvial Wedge Debris Flow Channel Deposit ? ? ? ?
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Martian Surface
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Clast Orientation Mars Statistics Eccentricity
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