By Richard H. Groshong
The booklet comprises new fabric, particularly examples of three-D types and methods for utilizing kinematic types to foretell fault and ramp-anticline geometry. The e-book is aimed toward the pro consumer fascinated with the accuracy of an interpretation and the rate with which it may be received from incomplete information. quite a few analytical strategies are provided that might be simply carried out with a pocket calculator or a spreadsheet.
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Extra resources for 3-D structural geology : a practical guide for surface and subsurfaces map interpretation
Determine the attitude of the eastern contact between the Mpm and the Mtfp by the 3-point method and from the structure contours. Are they the same? If they are different, discuss which answer is better. What would be the apparent dip of the Mpm in a north-south roadcut through the northwestern limb of the anticline? Fig. 26. Map grid for plotting points in a deviated well Fig. 27. Geological map of the northeast corner of the Blount Springs area, southern Appalachian fold-thrust belt. Thin lines are topographic contours (elevations in feet).
Dip domains have also been referred to as kink bands, but the term kink band has mechanical Fig. 11. Thickness (t). a Unit of constant thickness. b Unit of variable thickness Fig. 12. Regions of uniform dip properties. a Dip domains. b Concentric domains separated by a planar dip domain (shaded) 9 10 Chapter 1 · Elements of Map-Scale Structure implications that are not necessarily appropriate for every structure. An axial surface (Fig. 12a) is a surface that connects fold hinge lines, where a hinge line is a line of maximum curvature on the surface of a bed (Dennis 1967).
4. 2. Data from well 4835-B, Appleton field, Alabama. Kelly Bushing: 244 ft base of the Smackover. Plot the locations of the stratigraphic tops relative to the surface location of the well on the map (Fig. 26). Connect the points to show the shape of the well in map view. How far from the well (horizontally and in which direction) would you expect to first find the intersection of the oil-water contact with the top of the Smackover Formation, assuming constant dip for the Smackover? 2 Attitude Given the dip vector of the plane 35, 240, show on an overlay of a stereogram the trace of the plane, its dip vector, and its pole.
3-D structural geology : a practical guide for surface and subsurfaces map interpretation by Richard H. Groshong