stereonet | R Documentation |
Plots directional data on a Wulff or Schmidt stereonet. The Wulff equal angle polar Lambert projection preserves the shape of objects and is often used to visualise structural data. The Schmidt equal area polar Lambert projection preserves the size of objects and is more popular in mineralogy.
stereonet( trd, plg, coneAngle = rep(10, length(trd)), option = 1, wulff = TRUE, add = FALSE, degrees = FALSE, show.grid = TRUE, grid.col = "grey50", tl = 0.05, type = "p", labels = 1:length(trd), pch = 21, bg = c("black", "white"), lty = c(1, 2), ... )
trd |
trend angle, in degrees, between 0 and 360 (if
|
plg |
plunge angle, in degrees, between 0 and 90 (if
|
coneAngle |
if |
option |
scalar. If |
wulff |
logical. If |
add |
logical. If |
degrees |
logical. If |
show.grid |
logical. If |
grid.col |
colour of the grid. |
tl |
tick length for the N, E, S, W markers (value between 0 and 1). Set to 0 to omit the markers. |
type |
if |
labels |
if |
pch |
plot character: see ‘points’. |
bg |
background colours of the plot characters. Vector of two
colours, which are used to mark points that plot below and
above the projection plane of the stereonet, respectively. Only
relevant if |
lty |
line type. Vector of two numbers, which are used to plot lines below and above the projection plane of the stereonet, respectively. |
... |
optional arguments to be passed on to the generic
|
based on a MATLAB script written by Nestor Cardozo.
Allmendinger, R.W., Cardozo, N., and Fisher, D.M. “Structural geology algorithms: Vectors and tensors”. Cambridge University Press, 2011.
stereonet(trd=c(120,80),plg=c(10,30),degrees=TRUE,pch=16) stereonet(trd=c(120,80),plg=c(10,30),degrees=TRUE, option=4,coneAngle=c(5,10),add=TRUE)
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