bionic (1) psmeca.1gmt.gz

Provided by: gmt-common_5.4.3+dfsg-1_all bug

NAME

       psmeca - Plot focal mechanisms on maps

SYNOPSIS

       psmeca   [   table   ]   -Jparameters   -Rregion  [   -B[p|s]parameters  ]  [   -C[pen][Ppointsize]  ]  [
       -Ddepmin/depmax ] [  -Efill] [  -Fmode[args] ] [  -Gfill] [  -K ] [  -L[pen] ] [  -M ] [  -N ] [  -O ]  [
       -P  ]  [   -S<format><scale>[/d]]  [   -Tnum_of_plane[pen]  ]  [  -U[stamp] ] [  -V[level] ] [  -Wpen ] [
       -Xx_offset ] [  -Yy_offset ] [  -Zcpt] [ -dinodata ] [ -eregexp ] [ -hheaders ] [ -iflags ] [ -ttransp  ]
       [ -:[i|o] ]

       Note: No space is allowed between the option flag and the associated arguments.

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.

REQUIRED ARGUMENTS

       table  One  or  more  ASCII (or binary, see -bi[ncols][type]) data table file(s) holding a number of data
              columns. If no tables are given then we read from standard input.

       -Jparameters (more …)
              Select map projection.

       -Rwest/east/south/north[/zmin/zmax][+r][+uunit]
              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 for grid
              creation, give Rcodelon/lat/nx/ny, where code is a 2-character combination of L, C, R  (for  left,
              center, or right) and T, M, B for top, middle, or bottom. e.g., BL for lower left.  This indicates
              which point on a rectangular region the lon/lat coordinate refers to, and the grid  dimensions  nx
              and  ny  with  grid  spacings  via  -I is used to create the corresponding region.  Alternatively,
              specify the name of an existing grid file and the -R settings (and grid  spacing,  if  applicable)
              are  copied  from  the grid. Appending +uunit expects projected (Cartesian) coordinates compatible
              with chosen -J and we inversely project to determine actual rectangular  geographic  region.   For
              perspective  view (-p), optionally append /zmin/zmax.  In case of perspective view (-p), a z-range
              (zmin, zmax) can be appended to indicate the third dimension. This needs  to  be  done  only  when
              using  the -Jz option, not when using only the -p option. In the latter case a perspective view of
              the plane is plotted, with no third dimension.

       -S<format><scale>[/d]

       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, 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. Append u to
       have  the  text  appear  below  the  beach  ball (default is above). Parameters are expected to be in the
       following columns:
          1,2: longitude, latitude of event (-: option interchanges order)  3:  depth  of  event  in  kilometers
          4,5,6:  strike,  dip and rake in degrees 7: magnitude 8,9: 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).  10: Text string to appear above or below 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,  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. Append u to have the text appear below the beach ball (default  is  above).
       Parameters are expected to be in the following columns:
          1,2:  longitude,  latitude  of  event  (-:  option interchanges order) 3: depth of event in kilometers
          4,5,6: strike, dip, and rake of plane 1 7,8,9: strike, dip, and rake of plane 2  10,11:  mantissa  and
          exponent  of  moment  in  dyne-cm  12,13: 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).  14: Text string to appear above or below 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.  Append  u  to
       have  the  text  appear  below  the  beach  ball (default is above). Parameters are expected to be in the
       following columns:
          1,2: longitude, latitude of event (-: option interchanges order)  3:  depth  of  event  in  kilometers
          4,5,6,7,8,9:  mrr,  mtt,  mff,  mrt,  mrf,  mtf in 10*exponent dynes-cm 10: exponent 11,12: 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).  13:  Text  string  to
          appear above or below 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,  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.  Append
       u  to  have the text appear below the beach ball (default is above). Parameters are expected to be in the
       following columns:
          1,2: longitude, latitude of event (-: option interchanges order) 3: depth of event in kilometers  4,5:
          strike,  dip  of plane 1 6: strike of plane 2 7: must be -1/+1 for a normal/inverse fault 8: magnitude
          9,10: 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).   11:
          Text string to appear above or below 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, 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. Append u to
       have  the  text  appear  below  the  beach  ball (default is above). Parameters are expected to be in the
       following columns:
          1,2: longitude, latitude of event (-: option interchanges order)  3:  depth  of  event  in  kilometers
          4,5,6,7,8,9,10,11,12:  value (in 10*exponent dynes-cm), azimuth, plunge of T, N, P axis.  13: exponent
          14,15: 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).   16:
          Text string to appear above or below the beach ball (optional).

OPTIONAL ARGUMENTS

       -B[p|s]parameters (more …)
              Set map boundary frame and axes attributes.

       -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 as given by -W; pointsize 0].

       -Ddepmin/depmax
              Plots events between depmin and depmax.

       -Efill Selects filling of extensive quadrants. Usually white. Set the color [Default is white].

       -Fmode[args]
              Sets one or more attributes; repeatable. The various combinations are

       -Fa[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. [Default: 6p/cc]

       -Fefill
              Sets the color or fill pattern for the T axis symbol. [Default as set by -E]

       -Fgfill
              Sets the color or fill pattern for the P axis symbol. [Default as set by -G]

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

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

       -Fr[fill]
              Draw a box behind the label (if any). [Default fill is white]

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

       -Fz[pen]
              Overlay zero trace moment tensor using default pen (see -W), or sets pen attributes.

       -Gfill Selects filling of focal mechanisms. By convention,  the  compressional  quadrants  of  the  focal
              mechanism beach balls are shaded. Set the color [Default is black].

       -K (more …)
              Do not finalize the PostScript plot.

       -Lpen  Draws the “beach ball” outline with pen attributes instead of with the default pen set by -W.

       -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 (more …)
              Append to existing PostScript plot.

       -P (more …)
              Select “Portrait” plot orientation.

       -T[num_of_planes][/pen]
              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.

              Append /pen to set the pen attributes for this feature.  Default pen is as set by -W.

       -U[[just]/dx/dy/][c|label] (more …)
              Draw GMT time stamp logo on plot.

       -V[level] (more …)
              Select verbosity level [c].

       -Wpen  Set pen attributes for all lines and the outline of symbols [Defaults: width =  default,  color  =
              black,  style  =  solid]. This setting applies to -C, -L, -T, -p, -t, and -Fz, unless overruled by
              options to those arguments.

       -X[a|c|f|r][x-shift[u]]

       -Y[a|c|f|r][y-shift[u]] (more …)
              Shift plot origin.

       -Zcpt  Give a CPT and let compressive part color be determined by the z-value in the third column.

       -dinodata (more …)
              Replace input columns that equal nodata with NaN.

       -e[~]”pattern” | -e[~]/regexp/[i] (more …)
              Only accept data records that match the given pattern.

       -h[i|o][n][+c][+d][+rremark][+rtitle] (more …)
              Skip or produce header record(s).

       -icols[+l][+sscale][+ooffset][,] (more …)
              Select input columns and transformations (0 is first column).

       -t[transp] (more …)
              Set PDF transparency level in percent.

       -:[i|o] (more …)
              Swap 1st and 2nd column on input and/or output.

       -^ or just -
              Print a short message about the syntax of the command, then exits (NOTE: on Windows just use -).

       -+ or just +
              Print an extensive usage (help) message, including the explanation of any  module-specific  option
              (but not the GMT common options), then exits.

       -? or no arguments
              Print a complete usage (help) message, including the explanation of all options, then exits.

EXAMPLES

       The following file should give a normal-faulting CMT mechanism:

              gmt psmeca -R239/240/34/35.2 -Jm4c -Sc0.4 -h1 << 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

       pspolar, psvelo, pscoupe, gmt, psbasemap, psxy

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, Laboratory of Seismogenesis <http://www.ipgp.fr/rech/sismogenese/>, Institut de Physique
       du Globe de Paris, Departement de Sismologie, Paris, France

       2018, P. Wessel, W. H. F. Smith, R. Scharroo, J. Luis, and F. Wobbe