290 likes | 544 Views
Folds. Read Davis and Reynolds, Chapter 7. Why is it important? fundamental to deformation of the Earth’s crust; structural traps for oil ore deposits. Tectonic considerations. Folds, key to covergent margins, aid in resolving past stress regimes, crustal
E N D
Folds Read Davis and Reynolds, Chapter 7
Why is it important? • fundamental to deformation of the Earth’s crust; • structural traps for oil • ore deposits
Tectonic considerations Folds, key to covergent margins, aid in resolving past stress regimes, crustal shortening, closure of sedimentary basins. Sensitive markers to tectonic forces.
Relevance to oil and mining • Structural traps (anticlines are among the best traps • Folds control ore geometry especially in strata-bound deposits
Descriptive analysis • Basic definitions (anticline, syncline,overturned, etc.) • Geometric analysis (hinge, limb, axial plane, etc) • Specific geometries
Shapes of folds younger older • Anticlines, synclines • Antiform, synform • Anticlinorium, synclinorium younger old
Do not forget axial surface Hinge line Hinge, hinge zone Limb Axial plane Inflection point
Recumbent Fold lies on its side- typical for poly-deformed regions
Chevron Ptygmatic Cuspate
Geometry, size Heigth Median trace Width Amplitude Wavelength
Topographic Surfaces and folds
Layer thickness may change during folding Didn’t here- this is a “concentric” fold This one did- it is a “similar” fold
Fold tightness Gentle Angle is >90 degrees
tight (10ish degrees opening) to isoclinal (0 degrees)
Cylindrical (there is an axial surface) and non-cylindrical (too complex to have a defined axial surface) Poles to bedding Hinge line Hinge line readings
Example: Analyze this alpine example: Eocene Paleocene