# Cylindrical Folds - Field Geology - Lab handouts, Study notes for Geology

## Geology

Description: Following are the major entities discussed in this lab handout Cylindrical Folds, Down Plunges, Cross Sections, Apparent Dip, Maintain, Structures, Fold Axis, Planes Tangent, Beds, Lines Parallel
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1
DOWN PLUNGE CROSS SECTIONS
I Main Topics
A Cylindrical folds
B Downplunge cross-section views
C Apparent dip
II Cylindrical folds
A Surface of a cylindrical fold is parallel to a line called the fold axis.
B Cylindrical folds maintain their shape for “long” (infinite) distances in the
direction of the fold axis (as opposed to folds bending in the shape of a
bowl); they are two-dimensional structures because they do not change in
shape along the dimension of the fold axis.
C Planes tangent to cylindrically folded beds intersect in lines parallel to the
fold axis.
D Poles to cylindrically folded beds are contained in the plane perpendicular
to the fold axis, so taking the cross-product of the poles gives the
orientation of the fold axis.
III Down-plunge cross-section views
A Down-plunge cross-section views can be obtained directly from a geologic
map by looking obliquely at the map down a fold axis.
B Beds appear in true thickness
C Graphical technique
1 Find orientation of fold axis
2 Draw a cross-section along a plane parallel to the fold axis. The fold
axis will be contained in this plane and the fold axis will appear "in true
length" and its plunge can be measured.
3 Take an adjacent view of the above cross section where the line of
sight is parallel to the fold axis. Viewed end-on, the fold axis will
appear as a point. All the other lines lying in the surface of a
cylindrical fold will also be viewed end-on, so the fold surface will
appear as a curve.
D Computer-assisted technique using Matlab
1 Find three-dimensional coordinates of points on the folded units. This
can be done be digitizing a geologic map, for example, by scanning a
map and using Matlab’s ginput function:
[x,y] = ginput
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2
2 Transform the coordinates of the digitized points by projecting them
onto a new set of right-handed reference axes aligned with the fold
axis.
a “Manual” procedure
i Define the down-plunge (e.g., X,Y,Z) reference frame in terms of
the geographic (e.g., x,y,z) reference frame.
For example, let the Y axis be the down-plunge direction, the X
axis be horizontal and 90° clockwise from the fold axis trend,
and the Z axis be “up” (but not vertical). This is the view one
would get if you point you right arm and right index finger down
the fold axis, with your thumb pointing to the right. and your
middle finger pointing “up”.
ii Transform the coordinates from the x,y,z reference frame to the
X,Y,Z reference frame using the matrix transformation equations.
For one point:
X
Y
Z
=
a
Xx
a
Xy
a
Xz
a
Yx
a
Yy
a
Yz
a
Zx
a
Zy
a
Zz
x
y
z
(3x1) = (3x3) (3x1)
For n points:
X1X2... Xn
Y
1Y2... Yn
Z1Z2... Zn
=
aXx aXy aXz
aYx aYy aYz
aZx aZy aZz
x1x2... xn
y1y2... yn
z1z2... zn
(3xn) = (3x3) (3xn)
iii Then prepare an (X,Z) plot using Matlab’s plot command:
plot(X,Z)
The Y (down-plunge) coordinate is irrelevant for this view.
b “Automated Matlab 3-D visualization technique”
i Use the Matlab command
plot3(x,y,z)
ii Then use the “view” command to look down the fold axis
view(-trend,plunge)
(Here the trend and plunge are in degrees, not radians)
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Subject: Geology
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