1PSCOUPE(1)                   Generic Mapping Tools                  PSCOUPE(1)
2
3
4

NAME

6       pscoupe - Plot cross-sections of focal mechanisms.
7

SYNOPSIS

9       pscoupe  files  -Jparameters  -Rwest/east/south/north[r] -Aparameters [
10       -B[p|s]parameters ]  [ -Efill ] [ -Gfill ] [ -H[i][nrec] ]  [  -K  ]  [
11       -L[pen]  ]  [  -M  ]  [  -N ] [ -O ] [ -P ] [ -S<format><scale>[/d] ] [
12       -s<symbol><size>[/d] ] [ -Tn ] [ -U[just/dx/dy/][c|label] ] [  -V  ]  [
13       -Wpen ] [ -X[a|c|r][x-shift[u]] ] [ -Y[a|c|r][y-shift[u]] ] [ -Zcpt ] [
14       -a[size/[P_symbol/[T_symbol]]] ] [ -gfill ] [ -efill  ]  [  -ppen  ]  [
15       -tpen ] [ -:[i|o] ] [ -ccopies ]
16

DESCRIPTION

18       pscoupe  reads data values from files [or standard input] and generates
19       PostScript code that will plot symbols, lines or polygons on  a  cross-
20       section.   Focal  mechanisms   may  be specified and require additional
21       columns of data.  The PostScript code is written to standard output.
22
23       files list one or more file-names. If no files are given, pscoupe  will
24       read standard input.
25
26       A new file is created with the new coordinates (x, y) and the mechanism
27       (from lower focal half-sphere  for  horizontal  plane,  to  half-sphere
28       behind  a  vertical  plane).  When the plane is not horizontal, - north
29       direction becomes upwards steepest descent direction of the plane (u) -
30       east  direction becomes strike direction of the plane (s) - down direc‐
31       tion (= north^east) becomes u^s
32       Axis angles are defined in the same way as in horizontal plane  in  the
33       new system.
34       Moment  tensor (initially in r, t, f system that is up, south, east) is
35       defined in (-u^s, -u, s) system.  A  file  is  created  with  extracted
36       events.
37
38
39       -J     Selects  the  map  projection. Scale is UNIT/degree, 1:xxxxx, or
40              width in UNIT (upper case modifier).  UNIT is cm,  inch,  or  m,
41              depending on the MEASURE_UNIT setting in .gmtdefaults4, but this
42              can be overridden on the command line by appending c, i, or m to
43              the  scale/width  value.   When  central  meridian  is optional,
44              default is center of longitude  range  on  -R  option.   Default
45              standard  parallel  is  the equator.  For map height, max dimen‐
46              sion, or min dimension, append h, +, or - to the width,  respec‐
47              tively.
48              More details can be found in the psbasemap man pages.
49
50              CYLINDRICAL PROJECTIONS:
51
52              -Jclon0/lat0/scale (Cassini)
53              -Jcyl_stere/[lon0/[lat0/]]scale (Cylindrical Stereographic)
54              -Jj[lon0/]scale (Miller)
55              -Jm[lon0/[lat0/]]scale (Mercator)
56              -Jmlon0/lat0/scale (Mercator - Give meridian and standard paral‐
57              lel)
58              -Jo[a]lon0/lat0/azimuth/scale  (Oblique  Mercator  -  point  and
59              azimuth)
60              -Jo[b]lon0/lat0/lon1/lat1/scale (Oblique Mercator - two points)
61              -Joclon0/lat0/lonp/latp/scale  (Oblique  Mercator  -  point  and
62              pole)
63              -Jq[lon0/[lat0/]]scale (Cylindrical Equidistant)
64              -Jtlon0/[lat0/]scale (TM - Transverse Mercator)
65              -Juzone/scale (UTM - Universal Transverse Mercator)
66              -Jy[lon0/[lat0/]]scale (Cylindrical Equal-Area)
67
68              CONIC PROJECTIONS:
69
70              -Jblon0/lat0/lat1/lat2/scale (Albers)
71              -Jdlon0/lat0/lat1/lat2/scale (Conic Equidistant)
72              -Jllon0/lat0/lat1/lat2/scale (Lambert Conic Conformal)
73              -Jpoly/[lon0/[lat0/]]scale ((American) Polyconic)
74
75              AZIMUTHAL PROJECTIONS:
76
77              -Jalon0/lat0[/horizon]/scale (Lambert Azimuthal Equal-Area)
78              -Jelon0/lat0[/horizon]/scale (Azimuthal Equidistant)
79              -Jflon0/lat0[/horizon]/scale (Gnomonic)
80              -Jglon0/lat0[/horizon]/scale (Orthographic)
81              -Jglon0/lat0/altitude/azimuth/tilt/twist/Width/Height/scale
82              (General Perspective).
83              -Jslon0/lat0[/horizon]/scale (General Stereographic)
84
85              MISCELLANEOUS PROJECTIONS:
86
87              -Jh[lon0/]scale (Hammer)
88              -Ji[lon0/]scale (Sinusoidal)
89              -Jkf[lon0/]scale (Eckert IV)
90              -Jk[s][lon0/]scale (Eckert VI)
91              -Jn[lon0/]scale (Robinson)
92              -Jr[lon0/]scale (Winkel Tripel)
93              -Jv[lon0/]scale (Van der Grinten)
94              -Jw[lon0/]scale (Mollweide)
95
96              NON-GEOGRAPHICAL PROJECTIONS:
97
98              -Jp[a]scale[/origin][r|z] (Polar coordinates (theta,r))
99              -Jxx-scale[d|l|ppow|t|T][/y-scale[d|l|ppow|t|T]]  (Linear,  log,
100              and power scaling)
101
102       -R     west, east, south, and north specify the Region of interest, and
103              you    may    specify    them   in   decimal   degrees   or   in
104              [+-]dd:mm[:ss.xxx][W|E|S|N] format.  Append r if lower left  and
105              upper  right  map coordinates are given instead of w/e/s/n.  The
106              two shorthands -Rg and -Rd stand for global  domain  (0/360  and
107              -180/+180  in longitude respectively, with -90/+90 in latitude).
108              Alternatively, specify the name of an existing grid file and the
109              -R  settings  (and  grid spacing, if applicable) are copied from
110              the grid.  If frame is  defined  from  cross-section  parameters
111              (see  -A)  this  option  is  not taken into account, but must be
112              present.
113
114       -A  selects the cross-section.
115              -Aalon1/lat1/lon2/lat2/dip/p_width/dmin/dmax[f]
116              lon and lat are the longitude and latitude of  points  1  and  2
117              limiting the length of the cross-section.
118              dip is the dip of the plane on which the cross-section is made.
119              p_width is the width of the cross-section on each side of a ver‐
120              tical plane or above and under an oblique plane.
121              dmin and dmax are the distances  min  and  max  from  horizontal
122              plane, along steepest descent direction.
123              Add f to get the frame from the cross-section parameters.
124              -Ablon1/lat1/strike/p_length/dip/p_width/dmin/dmax[f]
125              lon1 and lat1 are the longitude and latitude of the beginning of
126              the cross-section.
127              strike is the azimuth of the direction of the cross-section.
128              p_length is the length along which the cross-section is made.
129              The other parameters are the same as for -Aa option.
130              -Acx1/y1/x2/y2/dip/p_width/dmin/dmax[f]
131              The same as -Aa option with x and y cartesian coordinates.
132              -Adx1/y1/strike/p_length/dip/p_width/dmin/dmax[f]
133              The same as -Ab option with x and y cartesian coordinates.
134
135       -S     selects the meaning of the columns in the data file and the fig‐
136              ure to be plotted.
137
138       -Sascale[/fontsize[/offset[u]]]
139              Focal  mechanisms in Aki and Richards convention.  scale adjusts
140              the scaling of the radius of the "beach  ball",  which  will  be
141              proportional to the magnitude.  The scale is the size for magni‐
142              tude = 5 in MEASURE_UNIT (unless c, i, m, or p  is  appended  to
143              indicate  that  the  size information is in units of cm, inches,
144              meters, or points, respectively).  Use the -T option  to  render
145              the  beach ball transparent by drawing only the nodal planes and
146              the circumference.  The color or shade of the compressive  quad‐
147              rants  can  be specified with the -G option.  The color or shade
148              of the extensive quadrants can be specified with the -E  option.
149              Parameters are expected to be in the following columns:
150
151
152       longitude, latitude of event (-: option interchanges order)
153
154       depth of event in kilometers
155
156       strike, dip and rake
157
158       magnitude
159
160       not used; can be 0 0; allows use of the psmeca file format
161
162       text string to appear above the beach ball (default) or under (add u).
163
164
165       -Scscale
166               Focal  mechanisms in Harvard CMT convention.  scale adjusts the
167               scaling of the radius of the "beach ball", which will  be  pro‐
168               portional to the magnitude. The scale is the size for magnitude
169               = 5 (that is M0 = 4E+23 dynes-cm.) in MEASURE_UNIT  (unless  c,
170               i, m, or p is appended to indicate that the size information is
171               in units of cm, inches, meters, or points, respectively).   Use
172               the  -T  option to render the beach ball transparent by drawing
173               only the nodal planes and the circumference. The color or shade
174               of  the  compressive  quadrants  can  be  specified with the -G
175               option.  The color or shade of the extensive quadrants  can  be
176               specified with the -E option.  Parameters are expected to be in
177               the following columns:
178
179       longitude, latitude of event (-: option interchanges order)
180
181       depth of event in kilometers
182
183       strike, dip, and slip of plane 1
184
185       strike, dip, and slip of plane 2
186
187       mantissa and exponent of  moment  in  dyne-cm  (if  magnitude  is  uses
188       instead  of  scalar  moment, magnitude is in column 10 and 0 must be in
189       column 11)
190
191       not used; can be 0 0; allows use of the psmeca file format
192
193       text string to appear above the beach ball (default) or under (add u).
194
195
196       -Spscale[/fontsize[/offset[u]]]
197                   Focal mechanisms given with partial data  on  both  planes.
198                   scale  adjusts  the  scaling  of  the  radius of the "beach
199                   ball", which will be proportional to  the  magnitude.   The
200                   scale is the size for magnitude = 5 in MEASURE_UNIT (unless
201                   c, i, m, or p is appended to indicate that the size  infor‐
202                   mation  is  in  units  of  cm,  inches,  meters, or points,
203                   respectively).  The color or shade of the compressive quad‐
204                   rants  can  be  specified with the -G option.  The color or
205                   shade of the extensive quadrants can be specified with  the
206                   -E  option.  Parameters are expected to be in the following
207                   columns:
208
209       longitude, latitude of event (-: option interchanges order)
210
211       depth
212
213       strike, dip of plane 1
214
215       strike of plane 2
216
217       must be -1/+1 for a normal/inverse fault
218
219       magnitude
220
221       not used; can be 0 0; allows use of the psmeca file format
222
223       text string to appear above the beach ball (default) or under (add u).
224
225
226       -Sm|d|zscale[/fontsize[/offset[u]]]
227                Seismic moment tensor (Harvard CMT, with zero  trace).   scale
228                adjusts  the  scaling of the radius of the "beach ball", which
229                will be proportional to the magnitude. The scale is  the  size
230                for  magnitude  =  5  (that  is  seismic scalar moment = 4E+23
231                dynes-cm) in MEASURE_UNIT (unless c, i, m, or p is appended to
232                indicate  that the size information is in units of cm, inches,
233                meters, or points, respectively).  (-T0 option  overlays  best
234                double  couple  transparently.)  Put  -Sdscale[/fontsize[/off‐
235                set[u]]] to plot the only double couple part of moment tensor.
236                Put  -Szscale[/fontsize[/offset[u]]]  to plot anisotropic part
237                of moment tensor (zero trace).  The color or shade of the com‐
238                pressive  quadrants  can be specified with the -G option.  The
239                color or shade of the extensive  quadrants  can  be  specified
240                with the -E option.  Parameters are expected to be in the fol‐
241                lowing columns:
242
243       longitude, latitude of event (-: option interchanges order)
244
245       depth of event in kilometers
246
247       mrr, mtt, mff, mrt, mrf, mtf in 10*exponent dynes-cm
248
249       exponent
250
251       Not used; can be 0 0; allows use of the psmeca file format
252
253       Text string to appear above the beach ball (default) or under (add u).
254
255
256       -Sxscale[/fontsize[/offset[u]]]
257                  Principal axis.  scale adjusts the scaling of the radius  of
258                  the  "beach  ball", which will be proportional to the magni‐
259                  tude. The scale is the size for magnitude = 5 (that is seis‐
260                  mic  scalar  moment  =  4*10e+23  dynes-cm)  in MEASURE_UNIT
261                  (unless c, i, m, or p is appended to indicate that the  size
262                  information  is  in  units of cm, inches, meters, or points,
263                  respectively).  (-T0  option  overlays  best  double  couple
264                  transparently.)  Put -Syscale[/fontsize[/offset[u]]] to plot
265                  the  only  double  couple  part  of  moment   tensor.    Put
266                  -Stscale[/fontsize[/offset[u]]]  to plot anisotropic part of
267                  moment tensor (zero trace).  The color or shade of the  com‐
268                  pressive quadrants can be specified with the -G option.  The
269                  color or shade of the extensive quadrants can  be  specified
270                  with  the  -E  option.  Parameters are expected to be in the
271                  following columns:
272
273       longitude, latitude of event (-: option interchanges order)
274
275       depth of event in kilometers
276
277       value (in 10*exponent dynes-cm), azimuth, plunge of the  T,  N,  and  P
278       axes.
279
280       exponent
281
282       longitude, latitude at which to place beach ball. Entries in these
283                     columns  are  necessary with the -C option.  Using 0,0 in
284                     columns 9 and 10 will plot the beach ball at  the  longi‐
285                     tude,  latitude  given in columns 1 and 2.  The -: option
286                     will interchange the order of columns (1,2) and (9,10).
287
288       Text string to appear above the beach ball (optional).
289
290       -ssymbol[size[/fontsize[/offset[u]]]
291                     selects a symbol instead of mechanism.  Choose  from  the
292                     following:  (c)  circle,  (d) diamond, (i) itriangle, (s)
293                     square, (t) triangle, (x) cross.  size is the symbol size
294                     in  MEASURE_UNIT  (unless  c,  i,  m, or p is appended to
295                     indicate that the size information is  in  units  of  cm,
296                     inches,  meters,  or points, respectively).  If size must
297                     be read, it must be in column 4 and the text string  will
298                     start  in column 5.  Parameters are expected to be in the
299                     following columns:
300
301       longitude, latitude of event (-: option interchanges order)
302
303       depth of event in kilometers
304
305       Text string to appear above the beach ball (default) or under (add u).
306

OPTIONS

308       No space between the option flag and the associated arguments.
309
310       -B     Sets map boundary annotation and  tickmark  intervals;  see  the
311              psbasemap man page for all the details.
312
313       -Efill Selects  filling of extensive quadrants. Usually white.  Set the
314              shade (0-255) or color (r/g/b) [Default is 255/255/255].
315
316       -Gfill Selects filling of focal mechanisms. By convention, the compres‐
317              sional  quadrants  are  shaded.   Set the shade (0-255) or color
318              (r/g/b)  [Default  is   0/0/0].    Optionally,   specify   -Gpi‐
319              con_size/pattern,  where  pattern  gives the number of the image
320              pattern (1-90) OR the name of a Sun rasterfile.  icon_size  sets
321              the  unit size in inches.  To invert black and white pixels, use
322              -GP instead of -Gp.  See Appendix E for information on  individ‐
323              ual patterns.
324
325       -H     Input file(s) has header record(s).  If used, the default number
326              of header records is N_HEADER_RECS.  Use -Hi if only input  data
327              should  have  header  records  [Default  will  write  out header
328              records if the input data have  them].  Blank  lines  and  lines
329              starting with # are always skipped.
330
331       -K     More  PostScript code will be appended later [Default terminates
332              the plot system].
333
334       -L[pen]
335              Draws the "beach ball" outline using current  pen  (see  -W)  or
336              sets pen attributes.
337
338       -M     Same size for any magnitude.
339
340       -N     Does  NOT  skip  symbols  that  fall outside map border [Default
341              plots points inside border only].
342
343       -O     Selects Overlay plot mode [Default initializes a new  plot  sys‐
344              tem].
345
346       -P     Selects Portrait plotting mode [Default is Landscape, see gmtde‐
347              faults to change this].
348
349       -T[num_of_planes]
350              Plots the nodal planes and outlines the bubble which  is  trans‐
351              parent.  If num_of_planes is
352                    0: both nodal planes are plotted;
353                    1: only the first nodal plane is plotted;
354                    2: only the second nodal plane is plotted [Default: 0].
355
356       -U     Draw Unix System time stamp on plot.  By adding just/dx/dy/, the
357              user may specify the justification of the stamp  and  where  the
358              stamp  should  fall on the page relative to lower left corner of
359              the plot.  For example, BL/0/0 will align the lower left  corner
360              of  the  time  stamp  with  the  lower  left corner of the plot.
361              Optionally, append a label, or c (which will  plot  the  command
362              string.).   The  GMT  parameters  UNIX_TIME,  UNIX_TIME_POS, and
363              UNIX_TIME_FORMAT can affect the appearance; see the  gmtdefaults
364              man page for details.  The time string will be in the locale set
365              by the environment variable TZ (generally local time).
366
367       -V     Selects verbose mode, which will send progress reports to stderr
368              [Default runs "silently"].
369
370       -W     set pen attributes for text string or default pen attributes for
371              fault plane edges. [Defaults: width = 1, color = 0/0/0,  texture
372              = solid].
373
374       -X -Y  Shift  plot origin relative to the current origin by (x-shift,y-
375              shift) and optionally append the length unit (c, i, m, p).   You
376              can  prepend a to shift the origin back to the original position
377              after plotting, or prepend  r [Default]  to  reset  the  current
378              origin  to the new location.  If -O is used then the default (x-
379              shift,y-shift) is (0,0), otherwise it is (r1i, r1i)  or  (r2.5c,
380              r2.5c).  Alternatively, give c to align the center coordinate (x
381              or y) of the plot with the center of the page based  on  current
382              page size.
383
384       -Zcptfile
385              Give  a  color  palette  file  and let compressive part color be
386              determined by the z-value in the third column.
387
388       -a[size/[P_axis_symbol/[T_axis_symbol]]]
389              Computes and plots P and T axes with symbols. Optionally specify
390              size and (separate) P and T axis symbols from the following: (c)
391              circle,  (d)  diamond,  (h)  hexagon,  (i)   inverse   triangle,
392              (p)point,  (s)  square,  (t)  triangle,  (x)  cross.  [Defaults:
393              0.2c/c/c or 0.08i/c/c.]
394
395       -efill Selects filling of T axis symbol.   Set  the  shade  (0-255)  or
396              color (r/g/b) [Default is color of extensive parts.]
397
398       -gfill Selects  filling  of  P  axis  symbol.  Set the shade (0-255) or
399              color (r/g/b) [Default is color of compressive parts.]
400
401       -p[pen]
402              Draws the P axis outline using current pen (see -W), or sets pen
403              attributes.
404
405       -t[pen]
406              Draws the T axis outline using current pen (see -W), or sets pen
407              attributes.
408
409       -:     Toggles between  (longitude,latitude)  and  (latitude,longitude)
410              input and/or output.  [Default is (longitude,latitude)].  Append
411              i to select input only or o to  select  output  only.   [Default
412              affects both].
413
414       -c     Specifies the number of plot copies. [Default is 1].
415

SEE ALSO

417       GMT(1), psbasemap(1), psmeca(1), psxy(1)
418
419

REFERENCES

421       Bomford, G., Geodesy, 4th ed., Oxford University Press, 1980.
422       Aki, K. and P. Richards, Quantitative Seismology, Freeman, 1980.
423       F. A. Dahlen and Jeroen Tromp, Theoretical Seismology, Princeton, 1998,
424       p.167.  Definition of scalar moment.
425       Cliff Frohlich, Cliff's Nodes Concerning Plotting Nodal Lines for P, Sh
426       and Sv
427       Seismological  Research Letters, Volume 67, Number 1, January-February,
428       1996
429       Thorne Lay, Terry C. Wallace, Modern Global Seismology, Academic Press,
430       1995, p.384.
431       W.H.  Press,  S.A. Teukolsky, W.T. Vetterling, B.P. Flannery, Numerical
432       Recipes in C, Cambridge University press (routine jacobi)
433
434

AUTHOR

436       Genevieve Patau
437       CNRS UMR 7580
438       Seismology Dept.
439       Institut de Physique du Globe de Paris
440       (patau@ipgp.jussieu.fr)
441
442
443
444GMT 4.5.6                         10 Mar 2011                       PSCOUPE(1)
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