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 ]  [ -Ffill ] [ -Gfill ] [ -H[i][nrec] ]  [  -K  ]  [
11       -L[pen]  ]  [  -M  ]  [  -N ] [ -O ] [ -P ] [ -S<symbol><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
74              AZIMUTHAL PROJECTIONS:
75
76              -Jalon0/lat0[/horizon]/scale (Lambert Azimuthal Equal-Area)
77              -Jelon0/lat0[/horizon]/scale (Azimuthal Equidistant)
78              -Jflon0/lat0[/horizon]/scale (Gnomonic)
79              -Jglon0/lat0[/horizon]/scale (Orthographic)
80              -Jglon0/lat0/altitude/azimuth/tilt/twist/Width/Height/scale
81              (General Perspective).
82              -Jslon0/lat0[/horizon][/slat]/scale (General Stereographic)
83
84              MISCELLANEOUS PROJECTIONS:
85
86              -Jh[lon0/]scale (Hammer)
87              -Ji[lon0/]scale (Sinusoidal)
88              -Jkf[lon0/]scale (Eckert IV)
89              -Jk[s][lon0/]scale (Eckert IV)
90              -Jn[lon0/]scale (Robinson)
91              -Jr[lon0/]scale (Winkel Tripel)
92              -Jv[lon0/]scale (Van der Grinten)
93              -Jw[lon0/]scale (Mollweide)
94
95              NON-GEOGRAPHICAL PROJECTIONS:
96
97              -Jp[a]scale[/origin][r|z] (Polar coordinates (theta,r))
98              -Jxx-scale[d|l|ppow|t|T][/y-scale[d|l|ppow|t|T]]  (Linear,  log,
99              and power scaling)
100
101       -R     west, east, south, and north specify the Region of interest, and
102              you    may    specify    them   in   decimal   degrees   or   in
103              [+-]dd:mm[:ss.xxx][W|E|S|N] format.  Append r if lower left  and
104              upper  right  map coordinates are given instead of w/e/s/n.  The
105              two shorthands -Rg and -Rd stand for global  domain  (0/360  and
106              -180/+180  in longitude respectively, with -90/+90 in latitude).
107              If frame is defined from cross-section parameters (see -A)  this
108              option is not taken into account, but must be present.
109
110       -A  selects the cross-section.
111              -Aalon1/lat1/lon2/lat2/dip/p_width/dmin/dmax[f]
112              lon  and  lat  are  the longitude and latitude of points 1 and 2
113              limiting the length ot the cross-section.
114              dip is the dip of the plane on which the cross-section is made.
115              p_width is the width of the cross-section on each side of a ver‐
116              tical plane or above and under an oblique plane.
117              dmin  and  dmax  are  the  distances min and max from horizontal
118              plane, along steepest descent direction.
119              Add f to get the frame from the cross-section parameters.
120              -Ablon1/lat1/strike/p_length/dip/p_width/dmin/dmax[f]
121              lon1 and lat1 are the longitude and latitude of the beginning of
122              the cross-section.
123              strike is the azimut of the direction of the cross-section.
124              p_length is the length along which the cross-section is made.
125              The other parameters are the same as for -Aa option.
126              -Acx1/y1/x2/y2/dip/p_width/dmin/dmax[f]
127              The same as -Aa option with x and y cartesian coordinates.
128              -Adx1/y1/strike/p_length/dip/p_width/dmin/dmax[f]
129              The same as -Ab option with x and y cartesian coordinates.
130
131       -S     selects the meaning of the columns in the data file and the fig‐
132              ure to be plotted.
133
134       -Sascale[/fontsize[/offset[u]]]
135              Focal mechanisms in Aki and Richard convention.   scale  adjusts
136              the  scaling  of  the  radius of the "beach ball", which will be
137              proportional to the magnitude.  The scale is the size for magni‐
138              tude  =  5  in MEASURE_UNIT (unless c, i, m, or p is appended to
139              indicate that the size information is in units  of  cm,  inches,
140              meters,  or  points, respectively).  Use the -T option to render
141              the beach ball transparent by drawing only the nodal planes  and
142              the  circumference.  The color or shade of the compressive quad‐
143              rants can be specified with the -G option.  The color  or  shade
144              of  the extensive quadrants can be specified with the -E option.
145              Parameters are expected to be in the following columns:
146
147
148       1,2:   longitude, latitude of event (-: option interchanges order)
149
150       3:     depth of event in kilometers
151
152       4,5,6: strike, dip and rake
153
154       7:     magnitude
155
156       8,9:   not used; can be 0 0; allows use of the psmeca file format
157
158       10:    text string to appear above the beach ball  (default)  or  under
159              (add u).
160
161
162       -Scscale
163              Focal  mechanisms  in Harvard CMT convention.  scale adjusts the
164              scaling of the radius of the "beach ball", which will be propor‐
165              tional to the magnitude. The scale is the size for magnitude = 5
166              (that is M0 = 4E+23 dynes-cm.) in MEASURE_UNIT (unless c, i,  m,
167              or  p  is  appended  to indicate that the size information is in
168              units of cm, inches, meters, or points, respectively).  Use  the
169              -T  option  to render the beach ball transparent by drawing only
170              the nodal planes and the circumference. The color  or  shade  of
171              the  compressive  quadrants can be specified with the -G option.
172              The color or shade of the extensive quadrants can  be  specified
173              with  the  -E option.  Parameters are expected to be in the fol‐
174              lowing columns:
175
176       1,2:   longitude, latitude of event (-: option interchanges order)
177
178       3:     depth of event in kilometers
179
180       4,5,6: strike, dip, and slip of plane 1
181
182       7,8,9: strike, dip, and slip of plane 2
183
184       10,11: mantissa and exponent of moment in dyne-cm (if magnitude is uses
185              instead  of  scalar moment, magnitude is in column 10 and 0 must
186              be in column 11)
187
188       12,13: not used; can be 0 0; allows use of the psmeca file format
189
190       14:    text string to appear above the beach ball  (default)  or  under
191              (add u).
192
193
194       -Spscale[/fontsize[/offset[u]]]
195              Focal  mechanisms given with partial data on both planes.  scale
196              adjusts the scaling of the radius of  the  "beach  ball",  which
197              will  be  proportional  to the magnitude.  The scale is the size
198              for magnitude = 5 in MEASURE_UNIT (unless  c,  i,  m,  or  p  is
199              appended  to  indicate  that the size information is in units of
200              cm, inches, meters, or  points,  respectively).   The  color  or
201              shade  of the compressive quadrants can be specified with the -G
202              option.  The color or shade of the extensive  quadrants  can  be
203              specified  with the -E option.  Parameters are expected to be in
204              the following columns:
205
206       1,2:   longitude, latitude of event (-: option interchanges order)
207
208       3:     depth
209
210       4,5:   strike, dip of plane 1
211
212       6:     strike of plane 2
213
214       7:     must be -1/+1 for a normal/inverse fault
215
216       8:     magnitude
217
218       9,10:  not used; can be 0 0; allows use of the psmeca file format
219
220       11:    text string to appear above the beach ball  (default)  or  under
221              (add u).
222
223
224       -Smscale[/fontsize[/offset[u]]]
225              Seismic  moment tensor.  scale adjusts the scaling of the radius
226              of the "beach ball", which will be proportional  to  the  magni‐
227              tude.  The  scale is the size for magnitude = 5 (that is seismic
228              scalar moment = 4E+23 dynes-cm) in MEASURE_UNIT (unless c, i, m,
229              or  p  is  appended  to indicate that the size information is in
230              units of cm, inches, meters,  or  points,  respectively).   (-T0
231              option   overlays   best   double   couple  transparently.)  Put
232              -Sdscale[/fontsize[/offset[u]]] to plot the only  double  couple
233              part  of  moment tensor.  Put -Szscale[/fontsize[/offset[u]]] to
234              plot anisotropic part of moment tensor (zero trace).  The  color
235              or  shade of the compressive quadrants can be specified with the
236              -G option.  The color or shade of the extensive quadrants can be
237              specified  with the -E option.  Parameters are expected to be in
238              the following columns:
239
240       1,2:   longitude, latitude of event (-: option interchanges order)
241
242       3:     depth of event in kilometers
243
244       4,5,6,7,8,9:
245              mrr, mtt, mff, mrt, mrf, mtf in 10*exponent dynes-cm
246
247       10:    exponent
248
249       11,12: Not used; can be 0 0; allows use of the psmeca file format
250
251       13:    Text string to appear above the beach ball  (default)  or  under
252              (add u).
253
254
255       -Sxscale[/fontsize[/offset[u]]]
256              Principal  axis.  scale adjusts the scaling of the radius of the
257              "beach ball", which will be proportional to the  magnitude.  The
258              scale  is  the  size  for  magnitude = 5 (that is seismic scalar
259              moment = 4*10e+23 dynes-cm) in MEASURE_UNIT (unless c, i, m,  or
260              p  is appended to indicate that the size information is in units
261              of cm, inches, meters, or points,  respectively).   (-T0  option
262              overlays  best double couple transparently.) Put -Syscale[/font‐
263              size[/offset[u]]] to plot the only double couple part of  moment
264              tensor.  Put -Stscale[/fontsize[/offset[u]]] to plot anisotropic
265              part of moment tensor (zero trace).  The color or shade  of  the
266              compressive  quadrants can be specified with the -G option.  The
267              color or shade of the extensive quadrants can be specified  with
268              the  -E  option.  Parameters are expected to be in the following
269              columns:
270
271       1,2:   longitude, latitude of event (-: option interchanges order)
272
273       3:     depth of event in kilometers
274
275       4,5,6,7,8,9,10,11,12:
276              value (in 10*exponent dynes-cm), azimuth, plunge of  the  T,  N,
277              and P axes.
278
279       13:    exponent
280
281       14,15: longitude,  latitude  at  which  to place beach ball. Entries in
282              these columns are necessary with the -C option.   Using  0,0  in
283              columns 9 and 10 will plot the beach ball at the longitude, lat‐
284              itude given in columns 1 and 2.  The -: option will  interchange
285              the order of columns (1,2) and (9,10).
286
287       16:    Text string to appear above the beach ball (optional).
288
289       -ssymbol[size[/fontsize[/offset[u]]]
290              selects  a symbol instead of mechanism.  Choose from the follow‐
291              ing: (c) circle, (d) diamond, (i)  itriangle,  (s)  square,  (t)
292              triangle,  (x)  cross.   size is the symbol size in MEASURE_UNIT
293              (unless c, i, m, or p is appended  to  indicate  that  the  size
294              information  is  in  units  of  cm,  inches,  meters, or points,
295              respectively).  If size must be read, it must be in column 4 and
296              the text string will start in column 5.  Parameters are expected
297              to be in the following columns:
298
299       1,2:   longitude, latitude of event (-: option interchanges order)
300
301       3:     depth of event in kilometers
302
303       4:     Text string to appear above the beach ball  (default)  or  under
304              (add u).
305

OPTIONS

307       No space between the option flag and the associated arguments.
308
309       -B     Sets  map  boundary  annotation  and tickmark intervals; see the
310              psbasemap man page for all the details.
311
312       -Efill Selects filling of extensive quadrants. Usually white.  Set  the
313              shade (0-255) or color (r/g/b) [Default is 255/255/255].
314
315       -Gfill Selects filling of focal mechanisms. By convention, the compres‐
316              sional quadrants are shaded.  Set the  shade  (0-255)  or  color
317              (r/g/b)   [Default   is   0/0/0].    Optionally,  specify  -Gpi‐
318              con_size/pattern, where pattern gives the number  of  the  image
319              pattern  (1-90) OR the name of a Sun rasterfile.  icon_size sets
320              the unit size in inches.  To invert black and white pixels,  use
321              -GP  instead of -Gp.  See Appendix E for information on individ‐
322              ual patterns.
323
324       -H     Input file(s) has Header record(s).  Number  of  header  records
325              can be changed by editing your .gmtdefaults4 file.  If used, GMT
326              default is 1 header record. Use -Hi if only  input  data  should
327              have  header  records  [Default will write out header records if
328              the input data have them]. Blank lines and lines starting with #
329              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 Jeoren Trom, 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 4.3.1                         15 May 2008                       PSCOUPE(1)
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