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Visualizing structures An introduction to the geometry of geological structures in the field
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Goals To familiarize you with the 3- dimensionality of geological structures in the field Provide you with simple rules to use in geologic mapping of structures
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3D spaces to deal with Topographic Depositional/intrusive Deformational They all intersect
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Shaded Non-shaded
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Any structures will intersect an irregular topography Try picturing how will a horizontal layer cut this relief
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Horizontal plane - follows topo contours
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Let us now put the real topography aside and step into the realm of “primary” geologic structures - layering of sedimentary units, intrusions, viewed in an idealized 3D framework
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Complicating the issue a little bit… Unconformity, what is it?
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Possible scenario: Deposition, erosion, deformation, new deposition
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The way this would look in a canyon near Page, AZ
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Igneous intrusions
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Structures on block diagrams
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Let us know try to drape structures onto topography and come up with some simple rules for the way they will plot on maps. To keep things simple for now, I will deal mainly with planes and not with lines. So what can a plane be? A bed, a fault, a dike, a sill an unconformity, anything that is planar.
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The simplest scenario: a horizontal bed
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Horizontal beds (a’la water line)
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Some shallow tilt of a plane
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Rule of v’s
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An example
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So then what is a geological map? An overlay of geologic structures (e.g. like the planes shown here on the 2D topographic map). Let’s take a look.
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Tucson Mts.
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Cross-sections
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Remember The 3 spaces you deal with: topo, primary structures and deformational (secondary) structures); Rule of v’s, overall topography/structure intersections of any planes A structure looks very different depending from where you look at it!
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