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II. Basic Techniques in Structural Geology
Field measurements and mapping Terminology on faults and folds Stereographic projections From maps to cross-sections Growth Strata Fault-related folds Seismic Imaging
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Two types of fault-related fold (drawn here assuming flexural slip folding)
Fault-bend fold Fault-propagation fold
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Fault-Bend Fold Fault Bend Folds (FBF) =ramp anticlines
throughgoing faults - slip is conserved. Fold amplitude is determined by the thickness above the lower hanging wall flat. Once the fold has achieved maximum amplitude, it only grows in width.
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Duplex system
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Thrust fault hangingwall and footwall ramps and flats…
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Fault-Propagation Fold Fault Propagation Folds (FPF)
fault slip is not conserved. Fault displacement is taken up by folding Fault tip is marked by a ductile ‘process zone’. Ideally, FPF’s evolve into FBF’s
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Fault-tip Folds Fault-propagation fold (non-parallel fold)
Detachment fold (folding is always non-parallel) Fault-propagation Fold (parallel fold)
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‘Drag folds’ Footwall rocks are commonly deformed into synclines
Could also relate to fault propagation
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Footwall syncline in the Canadian Cordillera
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Let’s practice…
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Primary strucure due to cross-bedding stratification
Primary strucure due to cross-bedding stratification. Not related to deformation
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Describe: from: http://earth.leeds.ac.uk/learnstructure/index.htm
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Recumbent tight similar syncline and anticline
similar fold parallel fold from: from: Recumbent tight similar syncline and anticline Upright open parallel syncline
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try to sketch: shallowly plunging, upright, tight, similar syncline
Assume fold axis plunges toward N45E
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Example from the Argentinian Cordillera
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What is it?
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Fault related Folds all from:
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Fault related Folds Fault-tip Fold Fault-bend Fold
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A case study of a fold and thrust belt: The North Tian Shan Piemont
(Charreau et al, 2008)
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Growth strata record of Kink Band migration (Huerguosi Anticline)
(Charreau et al, 2008) (Suppe et al., 1997; Hubert-Ferrari et al, 2007)
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Modeling 12 equations ex: Kinematic model (Charreau et al, 2008)
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(Charreau et al, 2008)
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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)
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Long Term History of Shortening
(Charreau et al, 2008)
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Sedimentation History
Accumulation rates– Piggy back Accumulation rates- magnetostratigraphy (Charreau et al, 2008)
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