1GRDSPOTTER(1)                Generic Mapping Tools               GRDSPOTTER(1)
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NAME

6       grdspotter - Create CVA image directly from gravity or bathymetry grids
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SYNOPSIS

9       grdspotter         [grdfile]         -Erotations_file         -GCVAgrid
10       -Ixinc[unit][=|+][/yinc[unit][=|+]] -Rwest/east/south/north[r] [ -Aage‐
11       grid  ] [ -Bn_try ] [ -C ] [ -DDIgrid ] [ -F ] [ -M ] [ -Nupper_age ] [
12       -PPAgrid ] [ -QIDinfo ] [ -S ] [  -T  ]  [  -Ufixed_val  ]  [  -V  ]  [
13       -Zz_min[/z_max[/z_inc]] ]
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DESCRIPTION

16       grdspotter  reads  a  grid file with residual bathymetry or gravity and
17       calculates flowlines from each node that exceeds a minimum value  using
18       the  specified rotations file.  These flowlines are then convolved with
19       the volume of the prism represented by each grid node and added  up  to
20       give a Cumulative Volcano Amplitude grid (CVA).
21            No  space  between  the  option flag and the associated arguments.
22       Use upper case for the option flags and lower case for modifiers.
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24       grdfile
25              Data grid to be  processed,  typically  residual  bathymetry  or
26              free-air anomalies.
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28       -E     Give  file  with  rotation  poles and opening angles.  This file
29              must contain one record for each stage; each record must  be  of
30              the following format:
31
32                   lon lat tstart tstop ccw-angle
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34              where  tstart  and  tstop  are in Ma and the rest is in degrees.
35              The oldest stage must be listed first.  tstart  (tstop)  is  the
36              age  of  the  old  (young)  end  of  the stage.  Blank lines and
37              records whose first column contains # will be ignored.  However,
38              see -C for total recostruction poles.
39
40       -G     Specify name for output CVA grid file.
41
42       -I     x_inc  [and  optionally  y_inc] is the grid spacing. Optionally,
43              append a suffix modifier.  Geographical  (degrees)  coordinates:
44              Append  m  to indicate arc minutes or c to indicate arc seconds.
45              If one of the units e, k, i,  or  n  is  appended  instead,  the
46              increment  is assumed to be given in meter, km, miles, or nauti‐
47              cal miles, respectively, and will be converted to the equivalent
48              degrees longitude at the middle latitude of the region (the con‐
49              version depends on ELLIPSOID).  If /y_inc is given but set to  0
50              it  will be reset equal to x_inc; otherwise it will be converted
51              to degrees latitude.  All coordinates: If = is appended then the
52              corresponding max x (east) or y (north) may be slightly adjusted
53              to fit exactly the given increment [by default the increment may
54              be adjusted slightly to fit the given domain].  Finally, instead
55              of giving an increment you  may  specify  the  number  of  nodes
56              desired  by  appending  +  to the supplied integer argument; the
57              increment is then recalculated from the number of nodes and  the
58              domain.   The  resulting  increment value depends on whether you
59              have selected a gridline-registered  or  pixel-registered  grid;
60              see Appendix B for details.
61
62       -R     west, east, south, and north specify the Region of interest, and
63              you   may   specify   them   in   decimal    degrees    or    in
64              [+-]dd:mm[:ss.xxx][W|E|S|N]  format.  Append r if lower left and
65              upper right map coordinates are given instead of  w/e/s/n.   The
66              two  shorthands  -Rg  and -Rd stand for global domain (0/360 and
67              -180/+180 in longitude respectively, with -90/+90 in latitude).
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OPTIONS

70       -A     Supply a crustal age grid that is co-registered with  the  input
71              data  grid.   These  ages become the upper ages to use when con‐
72              structing flowlines [Default extend flowlines back to oldest age
73              found in the rotation file; but see -N].
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75       -B     Get  n_try  bootstrap estimates of the maximum CVA location; the
76              longitude and latitude results are written to stdout [Default is
77              no bootstrapping].  Cannot be used with -M.
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79       -C     Expect  Total  Reconstruction  Poles  rather than Backward Stage
80              Poles [Default].  File format is similar to the stage pole  for‐
81              mat  except  the youngest rotation must be listed first and that
82              the tstart column is optional (assumed to be 0 Ma).
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84       -D     Use flowlines to determine the  maximum  CVA  encountered  along
85              each  flowline and create a Data Importance (DI) grid with these
86              values at the originating nodes.
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88       -F     Force pixel registration [Default is grid registration].
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90       -L     Supply a co-registered grid with seamount  chain  IDs  for  each
91              node.  This option requires that you also use -Q.
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93       -M     Do  not  attempt  to  keep all flowlines in memory when using -D
94              and/or -P.  Should you run out of memory you can use this option
95              to  compute  flowlines  on-the-fly.   It will be slower as we no
96              longer can reuse the flowlines  calculated  for  the  CVA  step.
97              Cannot be used with -B or the multi-slice mode in -Z.
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99       -N     Set  the  upper  age  to  assign  to  nodes whose crustal age is
100              unknown (i.e., NaN) [no upper age].  Also see -A.
101
102       -P     Use flowlines to determine the flowline age at the  CVA  maximum
103              for  each  node  and create a Predicted Age (PA) grid with these
104              values at the originating nodes.
105
106       -Q     Either give (1) a single ID to use or (2) the  name  of  a  file
107              with  a  list  of  IDs to use [Default uses all IDs].  Each line
108              would be TAG ID [w e s n].  The w/e/s/n zoom box is optional; if
109              specified  it  means  we  only trace the flowline if inside this
110              region [Default uses region set by -R].  Requires -L.
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112       -S     Normalize the resulting CVA grid to percentages of the CVA maxi‐
113              mum.  This also normalizes the DI grid (if requested).
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115       -T     Truncate  crustal  ages  given via the -A option that exceed the
116              upper age set with -N [no truncation].
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118       -U     After a node passes the test implied by -Z, use  this  fixed_val
119              instead in the calculations.  [Default uses individual node val‐
120              ues].
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122       -V     Selects verbose mode, which will send progress reports to stderr
123              [Default runs "silently"].
124
125       -Z     Ignore  nodes  with z-values lower than z_min [0] and optionally
126              larger than z_max [Inf].  Give z_min/z_max/z_inc to  make  sepa‐
127              rate  CVA  grids  for each z-slice [Default makes one CVA grid].
128              Multi-slicing cannot be used with -M.
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EXAMPLES

131       To  create   a   CVA   image   from   the   Pacific   topography   grid
132       Pac_res_topo.grd,  using the DC85.d Euler poles, and only output a grid
133       for the specified domain, run
134
135       grdspotter Pac_res_topo.grd  -EDC85.d  -GCVA.grd  -R190/220/15/25  -I2m
136       -N145 -T -V
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138       This file can then be plotted with grdimage.
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SEE ALSO

141       GMT(1),   grdimage(1),   project(1),   mapproject(1),   backtracker(1),
142       hotspotter(1), originator(1)
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REFERENCES

145       Wessel, P., 1999, "Hotspotting" tools  released,  EOS  Trans.  AGU,  80
146       (29), p. 319.
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150GMT 4.3.1                         15 May 2008                    GRDSPOTTER(1)
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