PoR_shmax {tectonicr} | R Documentation |
Direction of Maximum Horizontal Stress in PoR reference system
Description
Models the direction of maximum horizontal stress
\sigma_{Hmax}
in the Euler pole (Pole of Rotation)
coordinate reference system. When type of plate boundary is given, it also
gives the deviation from the theoretically predicted azimuth of
\sigma_{Hmax}
, the deviation, and the normalized
\chi^2
statistics.
Usage
PoR_shmax(df, PoR, type = c("none", "in", "out", "right", "left"))
Arguments
df |
|
PoR |
|
type |
Character. Type of plate boundary (optional). Can be
|
Details
The azimuth of \sigma_{Hmax}
in the pole of rotation
reference system is
approximate 0 (or 180), 45, 90, 135 degrees if the stress is sourced by an
outward, sinistral, inward, or dextral moving plate boundary, respectively.
directions of \sigma_{Hmax}
with respect to the four
plate boundary types.
Value
Either a numeric vector of the azimuths in the transformed coordinate
system (in degrees), or a "data.frame"
with
azi.PoR
the transformed azimuths (in degrees),
prd
the predicted azimuths (in degrees),
dev
the deviation between the transformed and the predicted azimuth (in degrees),
nchisq
the Norm
\chi^2
test statistic, andcdist
the angular distance between the transformed and the predicted azimuth.
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). doi:10.1038/s41598-023-42433-2.
See Also
model_shmax()
to compute the theoretical direction of
\sigma_{Hmax}
in the geographical reference system.
deviation_shmax()
to compute the deviation of the modeled direction
from the observed direction of \sigma_{Hmax}
.
norm_chisq()
to calculate the normalized \chi^2
statistics. circular_distance()
to calculate the angular distance.
Examples
data("nuvel1")
# North America relative to Pacific plate:
PoR <- subset(nuvel1, nuvel1$plate.rot == "na")
data("san_andreas")
res <- PoR_shmax(san_andreas, PoR, type = "right")
head(res)