PSCOUPE(1) Generic Mapping Tools PSCOUPE(1)NAMEpscoupe - Plot cross-sections of focal mechanisms.
SYNOPSISpscoupe files -Jparameters -Rwest/east/south/north[r] -Aparameters [
-B[p|s]parameters ] [ -Efill ] [ -Gfill ] [ -H[i][nrec] ] [ -K ] [
-L[pen] ] [ -M ] [ -N ] [ -O ] [ -P ] [ -S<format><scale>[/d] ] [
-s<symbol><size>[/d] ] [ -Tn ] [ -U[just/dx/dy/][c|label] ] [ -V ] [
-Wpen ] [ -X[a|c|r][x-shift[u]] ] [ -Y[a|c|r][y-shift[u]] ] [ -Zcpt ] [
-a[size/[P_symbol/[T_symbol]]] ] [ -gfill ] [ -efill ] [ -ppen ] [
-tpen ] [ -:[i|o] ] [ -ccopies ]
DESCRIPTIONpscoupe reads data values from files [or standard input] and generates
PostScript code that will plot symbols, lines or polygons on a cross-
section. Focal mechanisms may be specified and require additional
columns of data. The PostScript code is written to standard output.
files list one or more file-names. If no files are given, pscoupe will
read standard input.
A new file is created with the new coordinates (x, y) and the mechanism
(from lower focal half-sphere for horizontal plane, to half-sphere
behind a vertical plane). When the plane is not horizontal, - north
direction becomes upwards steepest descent direction of the plane (u) -
east direction becomes strike direction of the plane (s) - down direc‐
tion (= north^east) becomes u^s
Axis angles are defined in the same way as in horizontal plane in the
new system.
Moment tensor (initially in r, t, f system that is up, south, east) is
defined in (-u^s, -u, s) system. A file is created with extracted
events.
-J Selects the map projection. Scale is UNIT/degree, 1:xxxxx, or
width in UNIT (upper case modifier). UNIT is cm, inch, or m,
depending on the MEASURE_UNIT setting in .gmtdefaults4, but this
can be overridden on the command line by appending c, i, or m to
the scale/width value. When central meridian is optional,
default is center of longitude range on -R option. Default
standard parallel is the equator. For map height, max dimen‐
sion, or min dimension, append h, +, or - to the width, respec‐
tively.
More details can be found in the psbasemap man pages.
CYLINDRICAL PROJECTIONS:
-Jclon0/lat0/scale (Cassini)
-Jcyl_stere/[lon0/[lat0/]]scale (Cylindrical Stereographic)
-Jj[lon0/]scale (Miller)
-Jm[lon0/[lat0/]]scale (Mercator)
-Jmlon0/lat0/scale (Mercator - Give meridian and standard paral‐
lel)
-Jo[a]lon0/lat0/azimuth/scale (Oblique Mercator - point and
azimuth)
-Jo[b]lon0/lat0/lon1/lat1/scale (Oblique Mercator - two points)
-Joclon0/lat0/lonp/latp/scale (Oblique Mercator - point and
pole)
-Jq[lon0/[lat0/]]scale (Cylindrical Equidistant)
-Jtlon0/[lat0/]scale (TM - Transverse Mercator)
-Juzone/scale (UTM - Universal Transverse Mercator)
-Jy[lon0/[lat0/]]scale (Cylindrical Equal-Area)
CONIC PROJECTIONS:
-Jblon0/lat0/lat1/lat2/scale (Albers)
-Jdlon0/lat0/lat1/lat2/scale (Conic Equidistant)
-Jllon0/lat0/lat1/lat2/scale (Lambert Conic Conformal)
-Jpoly/[lon0/[lat0/]]scale ((American) Polyconic)
AZIMUTHAL PROJECTIONS:
-Jalon0/lat0[/horizon]/scale (Lambert Azimuthal Equal-Area)
-Jelon0/lat0[/horizon]/scale (Azimuthal Equidistant)
-Jflon0/lat0[/horizon]/scale (Gnomonic)
-Jglon0/lat0[/horizon]/scale (Orthographic)
-Jglon0/lat0/altitude/azimuth/tilt/twist/Width/Height/scale
(General Perspective).
-Jslon0/lat0[/horizon]/scale (General Stereographic)
MISCELLANEOUS PROJECTIONS:
-Jh[lon0/]scale (Hammer)
-Ji[lon0/]scale (Sinusoidal)
-Jkf[lon0/]scale (Eckert IV)
-Jk[s][lon0/]scale (Eckert VI)
-Jn[lon0/]scale (Robinson)
-Jr[lon0/]scale (Winkel Tripel)
-Jv[lon0/]scale (Van der Grinten)
-Jw[lon0/]scale (Mollweide)
NON-GEOGRAPHICAL PROJECTIONS:
-Jp[a]scale[/origin][r|z] (Polar coordinates (theta,r))
-Jxx-scale[d|l|ppow|t|T][/y-scale[d|l|ppow|t|T]] (Linear, log,
and power scaling)
-R west, east, south, and north specify the Region of interest, and
you may specify them in decimal degrees or in
[+-]dd:mm[:ss.xxx][W|E|S|N] format. Append r if lower left and
upper right map coordinates are given instead of w/e/s/n. The
two shorthands -Rg and -Rd stand for global domain (0/360 and
-180/+180 in longitude respectively, with -90/+90 in latitude).
Alternatively, specify the name of an existing grid file and the
-R settings (and grid spacing, if applicable) are copied from
the grid. If frame is defined from cross-section parameters
(see -A) this option is not taken into account, but must be
present.
-A selects the cross-section.
-Aalon1/lat1/lon2/lat2/dip/p_width/dmin/dmax[f]
lon and lat are the longitude and latitude of points 1 and 2
limiting the length of the cross-section.
dip is the dip of the plane on which the cross-section is made.
p_width is the width of the cross-section on each side of a ver‐
tical plane or above and under an oblique plane.
dmin and dmax are the distances min and max from horizontal
plane, along steepest descent direction.
Add f to get the frame from the cross-section parameters.
-Ablon1/lat1/strike/p_length/dip/p_width/dmin/dmax[f]
lon1 and lat1 are the longitude and latitude of the beginning of
the cross-section.
strike is the azimuth of the direction of the cross-section.
p_length is the length along which the cross-section is made.
The other parameters are the same as for -Aa option.
-Acx1/y1/x2/y2/dip/p_width/dmin/dmax[f]
The same as -Aa option with x and y cartesian coordinates.
-Adx1/y1/strike/p_length/dip/p_width/dmin/dmax[f]
The same as -Ab option with x and y cartesian coordinates.
-S selects the meaning of the columns in the data file and the fig‐
ure to be plotted.
-Sascale[/fontsize[/offset[u]]]
Focal mechanisms in Aki and Richards convention. scale adjusts
the scaling of the radius of the "beach ball", which will be
proportional to the magnitude. The scale is the size for magni‐
tude = 5 in MEASURE_UNIT (unless c, i, m, or p is appended to
indicate that the size information is in units of cm, inches,
meters, or points, respectively). Use the -T option to render
the beach ball transparent by drawing only the nodal planes and
the circumference. The color or shade of the compressive quad‐
rants can be specified with the -G option. The color or shade
of the extensive quadrants can be specified with the -E option.
Parameters are expected to be in the following columns:
longitude, latitude of event (-: option interchanges order)
depth of event in kilometers
strike, dip and rake
magnitude
not used; can be 0 0; allows use of the psmeca file format
text string to appear above the beach ball (default) or under (add u).
-Sc scale
Focal mechanisms in Harvard CMT convention. scale adjusts the
scaling of the radius of the "beach ball", which will be pro‐
portional to the magnitude. The scale is the size for magnitude
= 5 (that is M0 = 4E+23 dynes-cm.) in MEASURE_UNIT (unless c,
i, m, or p is appended to indicate that the size information is
in units of cm, inches, meters, or points, respectively). Use
the -T option to render the beach ball transparent by drawing
only the nodal planes and the circumference. The color or shade
of the compressive quadrants can be specified with the -G
option. The color or shade of the extensive quadrants can be
specified with the -E option. Parameters are expected to be in
the following columns:
longitude, latitude of event (-: option interchanges order)
depth of event in kilometers
strike, dip, and slip of plane 1
strike, dip, and slip of plane 2
mantissa and exponent of moment in dyne-cm (if magnitude is uses
instead of scalar moment, magnitude is in column 10 and 0 must be in
column 11)
not used; can be 0 0; allows use of the psmeca file format
text string to appear above the beach ball (default) or under (add u).
-Spscale[/fontsize[/offset[u]]]
Focal mechanisms given with partial data on both planes.
scale adjusts the scaling of the radius of the "beach
ball", which will be proportional to the magnitude. The
scale is the size for magnitude = 5 in MEASURE_UNIT (unless
c, i, m, or p is appended to indicate that the size infor‐
mation is in units of cm, inches, meters, or points,
respectively). The color or shade of the compressive quad‐
rants can be specified with the -G option. The color or
shade of the extensive quadrants can be specified with the
-E option. Parameters are expected to be in the following
columns:
longitude, latitude of event (-: option interchanges order)
depth
strike, dip of plane 1
strike of plane 2
must be -1/+1 for a normal/inverse fault
magnitude
not used; can be 0 0; allows use of the psmeca file format
text string to appear above the beach ball (default) or under (add u).
-Sm|d|zscale[/fontsize[/offset[u]]]
Seismic moment tensor (Harvard CMT, with zero trace). scale
adjusts the scaling of the radius of the "beach ball", which
will be proportional to the magnitude. The scale is the size
for magnitude = 5 (that is seismic scalar moment = 4E+23
dynes-cm) in MEASURE_UNIT (unless c, i, m, or p is appended to
indicate that the size information is in units of cm, inches,
meters, or points, respectively). (-T0 option overlays best
double couple transparently.) Put -Sdscale[/fontsize[/off‐
set[u]]] to plot the only double couple part of moment tensor.
Put -Szscale[/fontsize[/offset[u]]] to plot anisotropic part
of moment tensor (zero trace). The color or shade of the com‐
pressive quadrants can be specified with the -G option. The
color or shade of the extensive quadrants can be specified
with the -E option. Parameters are expected to be in the fol‐
lowing columns:
longitude, latitude of event (-: option interchanges order)
depth of event in kilometers
mrr, mtt, mff, mrt, mrf, mtf in 10*exponent dynes-cm
exponent
Not used; can be 0 0; allows use of the psmeca file format
Text string to appear above the beach ball (default) or under (add u).
-Sxscale[/fontsize[/offset[u]]]
Principal axis. scale adjusts the scaling of the radius of
the "beach ball", which will be proportional to the magni‐
tude. The scale is the size for magnitude = 5 (that is seis‐
mic scalar moment = 4*10e+23 dynes-cm) in MEASURE_UNIT
(unless c, i, m, or p is appended to indicate that the size
information is in units of cm, inches, meters, or points,
respectively). (-T0 option overlays best double couple
transparently.) Put -Syscale[/fontsize[/offset[u]]] to plot
the only double couple part of moment tensor. Put
-Stscale[/fontsize[/offset[u]]] to plot anisotropic part of
moment tensor (zero trace). The color or shade of the com‐
pressive quadrants can be specified with the -G option. The
color or shade of the extensive quadrants can be specified
with the -E option. Parameters are expected to be in the
following columns:
longitude, latitude of event (-: option interchanges order)
depth of event in kilometers
value (in 10*exponent dynes-cm), azimuth, plunge of the T, N, and P
axes.
exponent
longitude, latitude at which to place beach ball. Entries in these
columns are necessary with the -C option. Using 0,0 in
columns 9 and 10 will plot the beach ball at the longi‐
tude, latitude given in columns 1 and 2. The -: option
will interchange the order of columns (1,2) and (9,10).
Text string to appear above the beach ball (optional).
-ssymbol[size[/fontsize[/offset[u]]]
selects a symbol instead of mechanism. Choose from the
following: (c) circle, (d) diamond, (i) itriangle, (s)
square, (t) triangle, (x) cross. size is the symbol size
in MEASURE_UNIT (unless c, i, m, or p is appended to
indicate that the size information is in units of cm,
inches, meters, or points, respectively). If size must
be read, it must be in column 4 and the text string will
start in column 5. Parameters are expected to be in the
following columns:
longitude, latitude of event (-: option interchanges order)
depth of event in kilometers
Text string to appear above the beach ball (default) or under (add u).
OPTIONS
No space between the option flag and the associated arguments.
-B Sets map boundary annotation and tickmark intervals; see the
psbasemap man page for all the details.
-Efill Selects filling of extensive quadrants. Usually white. Set the
shade (0-255) or color (r/g/b) [Default is 255/255/255].
-Gfill Selects filling of focal mechanisms. By convention, the compres‐
sional quadrants are shaded. Set the shade (0-255) or color
(r/g/b) [Default is 0/0/0]. Optionally, specify -Gpi‐
con_size/pattern, where pattern gives the number of the image
pattern (1-90) OR the name of a Sun rasterfile. icon_size sets
the unit size in inches. To invert black and white pixels, use
-GP instead of -Gp. See Appendix E for information on individ‐
ual patterns.
-H Input file(s) has header record(s). If used, the default number
of header records is N_HEADER_RECS. Use -Hi if only input data
should have header records [Default will write out header
records if the input data have them]. Blank lines and lines
starting with # are always skipped.
-K More PostScript code will be appended later [Default terminates
the plot system].
-L[pen]
Draws the "beach ball" outline using current pen (see -W) or
sets pen attributes.
-M Same size for any magnitude.
-N Does NOT skip symbols that fall outside map border [Default
plots points inside border only].
-O Selects Overlay plot mode [Default initializes a new plot sys‐
tem].
-P Selects Portrait plotting mode [Default is Landscape, see gmtde‐
faults to change this].
-T[num_of_planes]
Plots the nodal planes and outlines the bubble which is trans‐
parent. If num_of_planes is
0: both nodal planes are plotted;
1: only the first nodal plane is plotted;
2: only the second nodal plane is plotted [Default: 0].
-U Draw Unix System time stamp on plot. By adding just/dx/dy/, the
user may specify the justification of the stamp and where the
stamp should fall on the page relative to lower left corner of
the plot. For example, BL/0/0 will align the lower left corner
of the time stamp with the lower left corner of the plot.
Optionally, append a label, or c (which will plot the command
string.). The GMT parameters UNIX_TIME, UNIX_TIME_POS, and
UNIX_TIME_FORMAT can affect the appearance; see the gmtdefaults
man page for details. The time string will be in the locale set
by the environment variable TZ (generally local time).
-V Selects verbose mode, which will send progress reports to stderr
[Default runs "silently"].
-W set pen attributes for text string or default pen attributes for
fault plane edges. [Defaults: width = 1, color = 0/0/0, texture
= solid].
-X -Y Shift plot origin relative to the current origin by (x-shift,y-
shift) and optionally append the length unit (c, i, m, p). You
can prepend a to shift the origin back to the original position
after plotting, or prepend r [Default] to reset the current
origin to the new location. If -O is used then the default (x-
shift,y-shift) is (0,0), otherwise it is (r1i, r1i) or (r2.5c,
r2.5c). Alternatively, give c to align the center coordinate (x
or y) of the plot with the center of the page based on current
page size.
-Z cptfile
Give a color palette file and let compressive part color be
determined by the z-value in the third column.
-a[size/[P_axis_symbol/[T_axis_symbol]]]
Computes and plots P and T axes with symbols. Optionally specify
size and (separate) P and T axis symbols from the following: (c)
circle, (d) diamond, (h) hexagon, (i) inverse triangle,
(p)point, (s) square, (t) triangle, (x) cross. [Defaults:
0.2c/c/c or 0.08i/c/c.]
-efill Selects filling of T axis symbol. Set the shade (0-255) or
color (r/g/b) [Default is color of extensive parts.]
-gfill Selects filling of P axis symbol. Set the shade (0-255) or
color (r/g/b) [Default is color of compressive parts.]
-p[pen]
Draws the P axis outline using current pen (see -W), or sets pen
attributes.
-t[pen]
Draws the T axis outline using current pen (see -W), or sets pen
attributes.
-: Toggles between (longitude,latitude) and (latitude,longitude)
input and/or output. [Default is (longitude,latitude)]. Append
i to select input only or o to select output only. [Default
affects both].
-c Specifies the number of plot copies. [Default is 1].
SEE ALSOGMT(1), psbasemap(1), psmeca(1), psxy(1)REFERENCES
Bomford, G., Geodesy, 4th ed., Oxford University Press, 1980.
Aki, K. and P. Richards, Quantitative Seismology, Freeman, 1980.
F. A. Dahlen and Jeroen Tromp, Theoretical Seismology, Princeton, 1998,
p.167. Definition of scalar moment.
Cliff Frohlich, Cliff's Nodes Concerning Plotting Nodal Lines for P, Sh
and Sv
Seismological Research Letters, Volume 67, Number 1, January-February,
1996
Thorne Lay, Terry C. Wallace, Modern Global Seismology, Academic Press,
1995, p.384.
W.H. Press, S.A. Teukolsky, W.T. Vetterling, B.P. Flannery, Numerical
Recipes in C, Cambridge University press (routine jacobi)
AUTHOR
Genevieve Patau
CNRS UMR 7580
Seismology Dept.
Institut de Physique du Globe de Paris
(patau@ipgp.jussieu.fr)
GMT 4.5.14 1 Nov 2015 PSCOUPE(1)
