Provided by: gmt_4.5.11-1build1_amd64 bug

NAME

       psmeca - Plot focal mechanisms on maps

SYNOPSIS

       psmeca  files  -Jparameters  -Rwest/east/south/north[r]  [  -B[p|s]parameters ] [ -C[pen][Ppointsize] ] [
       -Ddepmin/depmax ] [ -Efill] [ -Gfill] [ -H[i][nrec] ] [ -K ] [ -L[pen] ] [ -M ] [ -N ] [ -O ] [  -P  ]  [
       -S<format><scale>[/d]]  [  -Tnum_of_plane[pen]  ]  [  -U[just/dx/dy/][c|label]  ]  [  -V  ]  [  -Wpen ] [
       -X[a|c|r][x-shift[u]] ] [ -Y[a|c|r][y-shift[u]] ] [ -Zcptfile] [ -z ] [ -a[size[P_symbol[T_symbol]]] ]  [
       -gfill ] [ -efill ] [ -o ] [ -ppen ] [ -tpen ] [ -:[i|o] ] [ -ccopies ]

DESCRIPTION

       psmeca  reads  data  values  from  files [or standard input] and generates PostScript code that will plot
       focal mechanisms on a map.  Most options are the same as for psxy.  The PostScript  code  is  written  to
       standard output.

ARGUMENTS

       files List one or more file-names. If no files are given, psmeca will read standard input.

       -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 dimension, or min dimension, append h, +, or - to
              the width, respectively.
              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 parallel)
              -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.

       -S     Selects  the  meaning  of  the  columns  in the data file .  In order to use the same file to plot
              cross-sections, depth is in third column.   Nevertheless,  it  is  possible  to  use  "old  style"
              psvelomeca input files without depth in third column using the -o option.

       -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.  Scale is the size for magnitude = 5 in
              inch  (unless  c, i, m, or p is appended).  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 rake in degrees

              magnitude

              longitude, latitude at which to place beach ball. Entries in these
                      columns are necessary with the -C option.  Using 0,0 in columns 8  and  9  will  plot  the
                      beach  ball  at  the  longitude,  latitude  given  in columns 1 and 2.  The -: option will
                      interchange the order of columns (1,2) and (8,9).

              Text string to appear above the beach ball (optional).

       -Scscale[/fontsize[/offset[u]]]
              Focal mechanisms in Harvard CMT convention.  scale adjusts the scaling of the radius of the "beach
              ball",  which  will be proportional to the magnitude. Scale is the size for magnitude = 5 (that is
              M0 = 4.0E23 dynes-cm) in inch (unless c, i, m, or p is appended).  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 rake of plane 1

              strike, dip, and rake of plane 2

              mantissa and exponent of moment in dyne-cm

              longitude, latitude at which to place beach ball. Entries in these
                          columns are necessary with the -C option.  Using (0,0) in columns 12 and 13 will  plot
                          the  beach  ball  at  the longitude, latitude given in columns 1 and 2.  The -: option
                          will interchange the order of columns (1,2) and (12,13).

              Text string to appear above the beach ball (optional).

       -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. Scale is the size for magnitude = 5
              (that is scalar seismic moment = 4.0E23 dynes-cm) in inch (unless c, i,  m,  or  p  is  appended).
              (-T0  option  overlays best double couple transparently.)  Use -Sm to plot the Harvard CMT seismic
              moment tensor with zero trace.  Use -Sd to plot only the double couple part of moment tensor.  Use
              -Sz  to  plot  the  anisotropic  part  of  moment  tensor (zero trace).  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

              mrr, mtt, mff, mrt, mrf, mtf in 10*exponent dynes-cm

              exponent

              longitude, latitude at which to place beach ball. Entries in these
                         columns are necessary with the -C option.  Using (0,0) in columns 11 and 12  will  plot
                         the beach ball at the longitude, latitude given in columns 1 and 2.  The -: option will
                         interchange the order of columns (1,2) and (11,12).

              Text string to appear above the beach ball (optional).

       -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. Scale is the size for magnitude
              = 5 in inch (unless c, i, m, or p is appended).  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 of plane 1

              strike of plane 2

              must be -1/+1 for a normal/inverse fault

              magnitude

              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  longitude,  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).

       -Sx|y|tscale[/fontsize[/offset[u]]]
              Principal axis.  scale adjusts the scaling of the radius  of  the  "beach  ball",  which  will  be
              proportional  to the magnitude. Scale is the size for magnitude = 5 (that is seismic scalar moment
              = 4*10e+23 dynes-cm) in inch (unless c, i, m, or p is appended).  (-T0 option overlays best double
              couple  transparently.)   Use  -Sx  to plot standard Harvard CMT.  Use -Sy to plot only the double
              couple part of moment tensor.  Use -St to plot zero trace moment tensor.  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

              value (in 10*exponent dynes-cm), azimuth, plunge of T, N, P axis.

              exponent

              longitude, latitude at which to place beach ball. Entries in these
                            columns  are  necessary  with  the -C option.  Using (0,0) in columns 14 and 15 will
                            plot the beach ball at the longitude, latitude given in columns 1  and  2.   The  -:
                            option will interchange the order of columns (1,2) and (14,15).

              Text string to appear above the beach ball (optional).

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.

       -C[pen][Ppointsize]
              Offsets focal mechanisms to the longitude, latitude specified in the last two columns of the input
              file  before  the (optional) text string.  A small circle is plotted at the initial location and a
              line connects the beachball to the circle.  Specify pen and/or pointsize to change the line  style
              and/or size of the circle. [Defaults: pen width = 1, color = 0/0/0, texture = solid; pointsize 0].

       -Ddepmin/depmax
              Plots events between depmin and depmax.

       -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  compressional  quadrants  of  the  focal
              mechanism beach balls are shaded.  Set the shade (0-255) or color (r/g/b) [Default is 0/0/0].

       -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 with pen attributes.  [Defaults width = 1, color = 0/0/0, texture =
              solid].

       -M     Use the same size for any magnitude. Size is given with -S.

       -N     Does  NOT  skip  symbols  that  fall outside frame boundary specified by -R [Default plots symbols
              inside frame only].

       -O     Selects Overlay plot mode [Default initializes a new plot system].

       -P     Selects Portrait plotting mode [Default is Landscape, see gmtdefaults to change this].

       -T[num_of_planes]
              Plots the nodal planes and outlines the bubble which is transparent.  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.

       -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

   SPECIFYING PENS
       pen    The attributes of lines and symbol outlines as defined by pen  is  a  comma  delimetered  list  of
              width, color and texture, each of which is optional.  width can be indicated as a measure (points,
              centimeters, inches) or as faint, thin[ner|nest], thick[er|est], fat[ter|test], or  obese.   color
              specifies  a gray shade or color (see SPECIFYING COLOR below).  texture is a combination of dashes
              `-' and dots `.'.

       -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.

       -Zcptfile
              Give a color palette file and let compressive part color be determined by the z-value in the third
              column.

       -z     Overlay zero trace moment tensor.

       -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/cc or 0.08i/cc.]

       -efill Selects filling of T axis symbol.  Set the shade (0-255) or color (r/g/b). Default is white.

       -gfill Selects filling of P axis symbol.  Set the shade (0-255) or color (r/g/b). Default black.

       -o     Use the psvelomeca input format without depth in the third column.

       -p[pen]
              Draws the P axis outline using default pen (see -W), or sets pen attributes.

       -t[pen]
              Draws the T axis outline using default 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].

EXAMPLES

       The following file should give a normal-faulting CMT mechanism:
       psmeca -R 239/240/34/35.2 -Jm 4 -Sc 0.4 -H 1 <<END>! test.ps
       lon     lat    depth str dip slip  st dip slip mant exp plon plat
       239.384 34.556  12.  180  18  -88   0  72  -90  5.5  0   0    0
       END

SEE ALSO

       GMT(1), psbasemap(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.
       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)

AUTHORS

       Genevieve Patau
       CNRS UMR 7580
       Seismology Dept.
       Institut de Physique du Globe de Paris
       (patau@.ipgp.jussieu.fr)