Theoretical Direction of Maximum Horizontal Stress in the geographical reference system.
Theoretical Direction of Maximum Horizontal Stress in the geographical reference system.
Models the direction of maximum horizontal stress SHmax along great circles, small circles, and loxodromes at a given point or points according to the relative plate motion in the geographical coordinate reference system.
model_shmax(df, euler)
Arguments
df: data.frame containing the coordinates of the point(s) (lat, lon).
euler: "data.frame" or object of class "euler.pole"
containing the geographical coordinates of the Euler pole
Returns
data.frame
gc: Azimuth of modeled SHmax following great circles
sc: Small circles
ld.cw: Clockwise loxodromes
ld.ccw: Counter-clockwise loxodromes
Details
SHmax following great circles is the (initial) bearing between the given point and the pole of relative plate motion. SHmax along small circles, clockwise, and counter-clockwise loxodromes is 90degree, +45degree, and 135degree
(-45degree) to this great circle bearing, respectively.
Examples
data("nuvel1")# North America relative to Pacific plate:euler <- subset(nuvel1, nuvel1$plate.rot =="na")# the point where we mant to model the SHmax direction:point <- data.frame(lat =45, lon =20)model_shmax(point, euler)
References
Stephan, T., Enkelmann, E., and Kroner, U. "Analyzing the horizontal orientation of the crustal stress adjacent to plate boundaries". Sci Rep 13. 15590 (2023). tools:::Rd_expr_doi("10.1038/s41598-023-42433-2") .
See Also
deviation_shmax() to compute the deviation of the modeled direction from the observed direction of SHmax. PoR_shmax() to calculate the azimuth of SHmax