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Learn basic techniques and principles in structural geology, deformation mechanisms, continuum mechanics, and earthquake focal mechanisms in this course. Includes hands-on field measurements and mapping using stereographic projections.
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Class Outline • Deformation of the lithosphere, an overview • Basic Techniques in Structural Geology and Tectonics • Basic of Continuum mechanics- strain • Basic of Continuum mechanics- stress • Deformation Mechanism…
II. Basic Techniques in Structural Geology • Fundamental principles • Field measurements and mapping • Stereographic projections • …
Representations of lines and planes.. Line as a pole.. Plane as great circle..
Stereographic equal-angle projection (Wulff’s Stereonet) Lambert’s equal area projection (Schmidt;s stereonet)
Spherical coordinate frame… Polar Net (N is the pole of the coordinate net)
Stereographic nets (equal-angle nets or Wulff)’s stereonets) NB: Only half of the sphere is generally plotted Polar Net (polar axis vertical) Meridional Net (polar axis horizontal)
Equal-area nets- Schmidt Polar Net (polar axis vertical) Meridional Net (polar axis horizontal)
Projecting data… B(B’): 72,0 (252,0) C:72,45
B (B’): 72,0 (252,0) C:72,45 Q: 227, 43 (e.g., dip direction of a bed S: 47, 47 (pole to bedding defined by Q)
Fold axis of (Cylindrical) fold might be determined from the intersection of bedding planes.
Folded beddingas poles &as great circles.. β diagram n(n-1)/2 intersections Π diagram
Elastic Rebound Theory Interseismic strain (locked fault gets stressed) Co-seismic strain (fault failure during Earthquake Posterior to Last earthquake
Earthquake focal mechanisms will always have variations in polarity. Some stations will have first motion up, others first motion down.