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Fault related Folds. Fault-tip Fold. Fault-bend Fold. http://earth.leeds.ac.uk/learnstructure/index.htm. Example from the Argentinian Cordillera. What is it?. Primary strucure due to cross-bedding stratification. Not related to deformation. Fault related Folds.
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Fault related Folds Fault-tip Fold Fault-bend Fold http://earth.leeds.ac.uk/learnstructure/index.htm
Primary strucure due to cross-bedding stratification. Not related to deformation
Fault related Folds all from: http://earth.leeds.ac.uk/learnstructure/index.htm http://earth.leeds.ac.uk/learnstructure/index.htm
II. Fold modeling • Balanced cross section • Fault-related folds • Growth Strata
Growth and pre-growth strata • The assumption of beds with constant thickness holds generally for ‘pre-growth’ strata. Syntectonic deposition will induce lateral variations of bed thickness. Such strata are called ‘growth strata’.
Example: Structure of a Fault-bend fold with Growth strata Growth triangles (Suppe et al., 1997; Hubert-Ferrari et al, 2007)
foldscarp… buttress unconformity
A case study of a fold and thrust belt: The North Tian Shan Piemont (Charreau et al, 2008)
A case study of a fold and thrust belt: The North Tian Shan Piemont A B (Charreau et al, 2008)
Growth strata record of Kink Band migration (Huerguosi Anticline) A B (Charreau et al, 2008) (Suppe et al., 1997; Hubert-Ferrari et al, 2007)
Modeling 12 equations ex: Kinematic model (Charreau et al, 2008)
Modeling dip angles Bedding expected from the pure Fault-bend fold model Bedding measured in surface Bedding expected from the fault-bend fold model with growth strata (Charreau et al, 2008)
Long Term History of Shortening (Charreau et al, 2008)
Sedimentation History Accumulation rates– Piggy back Accumulation rates- magnetostratigraphy (Charreau et al, 2008)