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qs6testmars.dat
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# This is the input file of FORTRAN77 program "qseis06" for calculation of
# synthetic seismograms based on a layered halfspace earth model.
#
# by
# Rongjiang Wang <wang@gfz-potsdam.de>
# GeoForschungsZentrum Potsdam
# Telegrafenberg, D-14473 Potsdam, Germany
#
# Last modified: Potsdam, Nov., 2006
#
# = = = = = = = = = = = = = = = = = = = = = = = = = = = = = = = = = = = = = = =
# If not specified, SI Unit System is used overall!
#
# Coordinate systems:
# cylindrical (z,r,t) with z = downward,
# r = from source outward,
# t = azmuth angle from north to east;
# cartesian (x,y,z) with x = north,
# y = east,
# z = downward;
# = = = = = = = = = = = = = = = = = = = = = = = = = = = = = = = = = = = = = = =
#
# SOURCE PARAMETERS
# =================
# 1. source depth [km]
#------------------------------------------------------------------------------
60. |dble: source_depth;
#------------------------------------------------------------------------------
#
# RECEIVER PARAMETERS
# ===================
# 1. receiver depth [km]
# 2. switch for distance sampling role (1/0 = equidistant/irregular); switch
# for unit used (1/0 = km/deg)
# 3. number of receiver distances (or zero if given later with azimuths)
# 4. if equidistant, then start and end trace distance (> 0); else if > 0,
# distance list (please order the receiver distances from small to large).
# If zero receivers, no list here at all.
# 5. (reduced) time begin [sec] & length of time window [sec], number of time
# samples (<= 2*nfmax in qsglobal.h)
# 6. switch for unit of the following time reduction parameter: 1 = velocity
# [km/sec], 0 = slowness [sec/deg]; time reduction parameter
#------------------------------------------------------------------------------
0.000 |dble: receiver_depth;
0 1 |int: sw_equidistant, sw_d_unit;
0 |int: no_distances;
0 500.0 2048 |dble: t_start,t_window; int: no_t_samples;
1 0.0 |int: sw_t_reduce; dble: t_reduce;
#------------------------------------------------------------------------------
#
# WAVENUMBER INTEGRATION PARAMETERS
# =================================
# 1. select slowness integration algorithm (0 = suggested for full wave-field
# modelling; 1 or 2 = suggested when using a slowness window with narrow
# taper range - a technique for suppressing space-domain aliasing);
# 2. 4 parameters for low and high slowness (Note 1) cut-offs [s/km] with
# tapering: 0 < slw1 < slw2 defining cosine taper at the lower end, and 0 <
# slw3 < slw4 defining the cosine taper at the higher end. default values
# will be used in case of inconsistent input of the cut-offs (possibly with
# much more computational effort);
# 3. parameter for sampling rate of the wavenumber integration (1 = sampled
# with the spatial Nyquist frequency, 2 = sampled with twice higher than
# the Nyquist, and so on: the larger this parameter, the smaller the space-
# domain aliasing effect, but also the more computation effort);
# 4. the factor for suppressing time domain aliasing (> 0 and <= 1) (Note 2).
#------------------------------------------------------------------------------
0 |int: sw_algorithm;
0.000 0.000 0.0 0.0 |dble: slw(1-4);
4.00 |dble: sample_rate;
0.01 |dble: supp_factor;
#------------------------------------------------------------------------------
#
# OPTIONS FOR PARTIAL SOLUTIONS
# (only applied to the source-site structure)
# ===========================================
#
# 1. switch for filtering free surface effects (0 = with free surface, i.e.,
# do not select this filter; 1 = without free surface; 2 = without free
# surface but with correction on amplitude and wave form. Note switch 2
# can only be used for receivers at the surface)
# 2. switch for filtering waves with a shallow penetration depth (concerning
# their whole trace from source to receiver), penetration depth limit [km]
#
# if this option is selected, waves whose travel path never exceeds the
# given depth limit will be filtered ("seismic nuting"). the condition for
# selecting this filter is that the given shallow path depth limit should
# be larger than both source and receiver depth.
#
# 3. number of depth ranges where the following selected up/down-sp2oing P or
# SV waves should be filtered
# 4. the 1. depth range: upper and lower depth [km], switch for filtering P
# or SV wave in this depth range:
#
# switch no: 1 2 3 4 other
# filtered phase: P(up) P(down) SV(up) SV(down) Error
#
# 5. the 2. ...
#
# The partial solution options are useful tools to increase the numerical
# significance of desired wave phases. Especially when the desired phases
# are smaller than the undesired phases, these options should be selected
# and carefully combined.
#------------------------------------------------------------------------------
0 |int: isurf;
0 560.0 |int: sw_path_filter; dble:shallow_depth_limit;
0 |int: no_of_depth_ranges;
# 2
# 0.0 5153.0 3
# 0.0 5153.0 4
#------------------------------------------------------------------------------
#
# SOURCE TIME FUNCTION (WAVELET) PARAMETERS (Note 3)
# ==================================================
# 1. wavelet duration [unit = time sample rather than sec!], that is about
# equal to the half-amplitude cut-off period of the wavelet (> 0. if <= 0,
# then default value = 2 time samples will be used), and switch for the
# wavelet form (0 = user's own wavelet; 1 = default wavelet: normalized
# square half-sinusoid for simulating a physical delta impulse; 2 = tapered
# Heaviside wavelet, i.e. integral of wavelet 1)
# 2. IF user's own wavelet is selected, then number of the wavelet time samples
# (<= 1024), and followed by
# 3. equidistant wavelet time samples
# 4 ...(continue) (! no comment lines allowed between the time sample list!)
# IF default, delete line 2, 3, 4 ... or comment them out!
#------------------------------------------------------------------------------
20. 1 |int:dble: wavelet_duration; sw_wavelet;
# 100 |int: no_w_samples; below dble: w_samples;
# 0.000 0.063 0.127 0.189 0.251 0.312 0.372 0.430 0.486 0.541
# 0.593 0.643 0.690 0.735 0.776 0.815 0.850 0.881 0.910 0.934
# 0.955 0.972 0.985 0.994 0.999 1.000 0.997 0.990 0.979 0.964
# 0.945 0.922 0.896 0.866 0.833 0.796 0.756 0.713 0.667 0.618
# 0.567 0.514 0.458 0.401 0.342 0.282 0.220 0.158 0.095 0.032
# -0.032 -0.095 -0.158 -0.220 -0.282 -0.342 -0.401 -0.458 -0.514 -0.567
# -0.618 -0.667 -0.713 -0.756 -0.796 -0.833 -0.866 -0.896 -0.922 -0.945
# -0.964 -0.979 -0.990 -0.997 -1.000 -0.999 -0.994 -0.985 -0.972 -0.955
# -0.934 -0.910 -0.881 -0.850 -0.815 -0.776 -0.735 -0.690 -0.643 -0.593
# -0.541 -0.486 -0.430 -0.372 -0.312 -0.251 -0.189 -0.127 -0.063 0.000
#------------------------------------------------------------------------------
#
# FILTER PARAMETERS OF RECEIVERS (SEISMOMETERS OR HYDROPHONES)
# ============================================================
# 1. constant coefficient (normalization factor)
# 2. number of roots (<= nrootmax in qsglobal.h)
# 3. list of the root positions in the complex format (Re,Im). If no roots,
# comment out this line
# 4. number of poles (<= npolemax in qsglobal.h)
# 5. list of the pole positions in the complex format (Re,Im). If no poles,
# comment out this line
#------------------------------------------------------------------------------
1.0
0
# (0.0, 0.0), (0.0, 0.0)
0
# (-4.35425, 4.44222), (-4.35425,-4.44222)
#------------------------------------------------------------------------------
#
# OUTPUT FILES FOR GREEN'S FUNCTIONS (Note 4)
# ===========================================
# 1. selections of source types (yes/no = 1/0)
# 2. file names of Green's functions (please give the names without extensions,
# which will be appended by the program automatically: *.tz, *.tr, *.tt
# and *.tv are for the vertical, radial, tangential, and volume change (for
# hydrophones) components, respectively)
#------------------------------------------------------------------------------
# explosion strike-slip dip-slip clvd single_f_v single_f_h
#------------------------------------------------------------------------------
1 0 0 0 0 0 |int
'mex' 'mss' 'mds' 'mcl' 'mfz' 'mfh' |char
#------------------------------------------------------------------------------
# OUTPUT FILES FOR AN ARBITRARY POINT DISLOCATION SOURCE
# (for applications to earthquakes)
# ======================================================
# 1. selection (0 = not selected; 1 or 2 = selected), if (selection = 1), then
# the 6 moment tensor elements [N*m]: Mxx, Myy, Mzz, Mxy, Myz, Mzx (x is
# northward, y is eastward and z is downard); else if (selection = 2), then
# Mis [N*m] = isotropic moment part = (MT+MN+MP)/3, Mcl = CLVD moment part
# = (2/3)(MT+MP-2*MN), Mdc = double-couple moment part = MT-MN, Strike [deg],
# Dip [deg] and Rake [deg].
#
# Note: to use this option, the Green's functions above should be computed
# (selection = 1) if they do not exist already.
#
# north(x)
# /
# /\ strike
# *-----------------------> east(y)
# |\ \
# |-\ \
# | \ fault plane \
# |90 \ \
# |-dip\ \
# | \ \
# | \ \
# downward(z) \-----------------------\
#
# 2. switch for azimuth distribution of the stations (0 = uniform azimuth,
# 1 = irregular azimuth angles). If no_distances (in RECEIVER PARAMETERS)
# is zero, the following list (item 3) of distances azimuths defines the
# total number of receivers.
# 3. list of the azimuth angles [deg] for all stations given above (if the
# uniform azimuth is selected, then only one azimuth angle is required).
# If no_distances (in RECEIVER PARAMETERS) is zero, a list of distance,
# azimuth and station name for each receiver follows, one per line. The
# list ends with a distance AND azimuth <= 0 (no count is needed).
#
#------------------------------------------------------------------------------
# Mis Mcl Mdc Strike Dip Rake File
#------------------------------------------------------------------------------
2 6.0E19 0.00 0.00 120.0 30.0 25.0 'mex'
#------------------------------------------------------------------------------
# Mxx Myy Mzz Mxy Myz Mzx File
#------------------------------------------------------------------------------
# 1 -0.36e+019 -5.12e+019 5.48e+019 -6.21e+019 2.40e+019 -3.84e+019 'mseis'
1
0 15 D00K
1 30 D01K
2 45 D02K
3 60 D03K
4 75 D04K
5 90 D05K
10 0 D10K
50 180 D50K
0 0 END
#------------------------------------------------------------------------------
#
# GLOBAL MODEL PARAMETERS (Note 5)
# ================================
# 1. switch for flat-earth-transform (1 = on, 0 = off) and [optional] planet
# radius (Earth assumed).
# 2. gradient resolution [%] of vp, vs, and ro (density), if <= 0, then default
# values (depending on wave length at cut-off frequency) will be used
#------------------------------------------------------------------------------
0 3390.0 |int: sw_flat_earth_transform; dble: radius
0.25 0.25 5.0 |dble: vp_res, vs_res, ro_res;
#------------------------------------------------------------------------------
#
# LAYERED EARTH MODEL
# (SHALLOW SOURCE + UNIFORM DEEP SOURCE/RECEIVER STRUCTURE)
# =========================================================
# 1. number of data lines of the layered model (source site)
#------------------------------------------------------------------------------
150 |int: no_model_lines;
#------------------------------------------------------------------------------
#
# MULTILAYERED MODEL PARAMETERS (source site) (Mars, Fo73 olivine mantle)
# =======================================================================
# no depth[km] vp[km/s] vs[km/s] ro[g/cm^3] qp qs
#------------------------------------------------------------------------------
1 0.0000 7.25860 3.48692 3.56503 10000.000 10000.000
2 5.0079 7.99143 4.54343 3.56159 10000.000 10000.000
3 10.0075 7.96918 4.52633 3.55726 10000.000 10000.000
4 15.0071 7.94439 4.50737 3.55236 10000.000 10000.000
5 20.0067 7.91785 4.48715 3.54706 10000.000 10000.000
6 25.0063 7.89002 4.46603 3.54148 10000.000 10000.000
7 30.0059 7.86117 4.44420 3.53566 10000.000 10000.000
8 35.0054 7.83147 4.42180 3.52967 10000.000 10000.000
9 40.0050 7.80104 4.39892 3.52350 10000.000 10000.000
10 45.0046 7.76993 4.37562 3.51719 10000.000 10000.000
11 50.0042 7.73818 4.35193 3.51075 10000.000 10000.000
12 55.0038 7.70583 4.32787 3.50418 10000.000 10000.000
13 60.0034 7.67288 4.30347 3.49748 10000.000 10000.000
14 65.0029 7.63933 4.27873 3.49065 10000.000 10000.000
15 70.0025 7.60517 4.25365 3.48371 10000.000 10000.000
16 75.0021 7.57039 4.22824 3.47664 10000.000 10000.000
17 80.0017 7.53498 4.20250 3.46943 10000.000 10000.000
18 85.0013 7.49890 4.17641 3.46210 10000.000 10000.000
19 90.0008 7.46213 4.14998 3.45464 10000.000 10000.000
20 95.0004 7.42461 4.12319 3.44703 10000.000 10000.000
21 100.0000 7.38633 4.09603 3.43928 10000.000 10000.000
22 100.0000 7.38619 4.09594 3.43925 10000.000 10000.000
23 111.4033 7.39779 4.10052 3.44360 10000.000 10000.000
24 122.8066 7.40929 4.10506 3.44792 10000.000 10000.000
25 134.2099 7.42071 4.10956 3.45222 10000.000 10000.000
26 145.6131 7.43203 4.11402 3.45651 10000.000 10000.000
27 157.0319 7.44328 4.11844 3.46077 10000.000 10000.000
28 168.4529 7.45444 4.12283 3.46502 10000.000 10000.000
29 179.8739 7.46553 4.12717 3.46924 10000.000 10000.000
30 191.2949 7.47652 4.13148 3.47345 10000.000 10000.000
31 202.7160 7.48744 4.13575 3.47764 10000.000 10000.000
32 214.1369 7.49829 4.13999 3.48181 10000.000 10000.000
33 225.5580 7.50905 4.14419 3.48596 10000.000 10000.000
34 236.9790 7.51974 4.14836 3.49009 10000.000 10000.000
35 248.4000 7.53036 4.15249 3.49420 10000.000 10000.000
36 259.8210 7.54091 4.15658 3.49830 10000.000 10000.000
37 271.2420 7.55138 4.16064 3.50238 10000.000 10000.000
38 282.6631 7.56179 4.16467 3.50644 10000.000 10000.000
39 294.0853 7.57211 4.16867 3.51049 10000.000 10000.000
40 305.5235 7.58237 4.17263 3.51452 10000.000 10000.000
41 316.9617 7.59256 4.17656 3.51853 10000.000 10000.000
42 328.3999 7.60269 4.18046 3.52253 10000.000 10000.000
43 339.8382 7.61276 4.18432 3.52651 10000.000 10000.000
44 351.2765 7.62275 4.18816 3.53047 10000.000 10000.000
45 362.7147 7.63269 4.19196 3.53442 10000.000 10000.000
46 374.1530 7.64256 4.19573 3.53836 10000.000 10000.000
47 385.5912 7.65237 4.19948 3.54227 10000.000 10000.000
48 397.0294 7.66211 4.20319 3.54618 10000.000 10000.000
49 408.4677 7.67180 4.20687 3.55006 10000.000 10000.000
50 419.9060 7.68143 4.21053 3.55394 10000.000 10000.000
51 431.3442 7.69100 4.21415 3.55780 10000.000 10000.000
52 442.8021 7.70050 4.21775 3.56164 10000.000 10000.000
53 454.2670 7.70996 4.22131 3.56547 10000.000 10000.000
54 465.7320 7.71935 4.22485 3.56929 10000.000 10000.000
55 477.1970 7.72869 4.22837 3.57309 10000.000 10000.000
56 488.6619 7.73797 4.23185 3.57688 10000.000 10000.000
57 500.1269 7.74719 4.23531 3.58065 10000.000 10000.000
58 511.5919 7.75638 4.23874 3.58441 10000.000 10000.000
59 523.0569 7.76550 4.24214 3.58816 10000.000 10000.000
60 534.5218 7.77456 4.24552 3.59190 10000.000 10000.000
61 545.9868 7.78358 4.24887 3.59562 10000.000 10000.000
62 557.4518 7.79254 4.25220 3.59932 10000.000 10000.000
63 568.9168 7.80145 4.25549 3.60302 10000.000 10000.000
64 580.4085 7.81032 4.25877 3.60670 10000.000 10000.000
65 591.9028 7.81914 4.26202 3.61037 10000.000 10000.000
66 603.3971 7.82790 4.26524 3.61403 10000.000 10000.000
67 614.8913 7.83662 4.26844 3.61768 10000.000 10000.000
68 626.3856 7.84529 4.27161 3.62131 10000.000 10000.000
69 637.8798 7.85390 4.27476 3.62493 10000.000 10000.000
70 649.3741 7.86248 4.27789 3.62854 10000.000 10000.000
71 660.8684 7.87101 4.28099 3.63214 10000.000 10000.000
72 672.3626 7.87949 4.28407 3.63572 10000.000 10000.000
73 683.8569 7.88792 4.28712 3.63930 10000.000 10000.000
74 695.3512 7.89631 4.29015 3.64286 10000.000 10000.000
75 706.8621 7.90466 4.29316 3.64641 10000.000 10000.000
76 718.3818 7.91295 4.29615 3.64995 10000.000 10000.000
77 729.9015 7.92121 4.29911 3.65348 10000.000 10000.000
78 741.4212 7.92943 4.30205 3.65700 10000.000 10000.000
79 752.9410 7.93759 4.30497 3.66051 10000.000 10000.000
80 764.4607 7.94571 4.30786 3.66400 10000.000 10000.000
81 775.9804 7.95381 4.31074 3.66749 10000.000 10000.000
82 787.5002 7.96185 4.31359 3.67096 10000.000 10000.000
83 799.0198 7.96985 4.31642 3.67443 10000.000 10000.000
84 810.5396 7.97782 4.31923 3.67788 10000.000 10000.000
85 822.0593 7.98573 4.32202 3.68132 10000.000 10000.000
86 833.5945 7.99362 4.32478 3.68476 10000.000 10000.000
87 845.1297 8.00145 4.32753 3.68818 10000.000 10000.000
88 856.6648 8.00926 4.33025 3.69159 10000.000 10000.000
89 868.2000 8.01703 4.33296 3.69499 10000.000 10000.000
90 879.7352 8.02475 4.33564 3.69839 10000.000 10000.000
91 891.2704 8.03243 4.33831 3.70177 10000.000 10000.000
92 902.8056 8.04008 4.34095 3.70514 10000.000 10000.000
93 914.3407 8.04769 4.34357 3.70850 10000.000 10000.000
94 925.8768 8.05527 4.34617 3.71186 10000.000 10000.000
95 937.4120 8.06281 4.34876 3.71520 10000.000 10000.000
96 948.9485 8.07030 4.35132 3.71853 10000.000 10000.000
97 960.4850 8.07778 4.35387 3.72186 10000.000 10000.000
98 972.0215 8.08520 4.35639 3.72518 10000.000 10000.000
99 983.5581 8.09259 4.35890 3.72848 10000.000 10000.000
100 995.0946 8.12558 4.37718 3.73412 10000.000 10000.000
101 1006.6311 8.19039 4.41257 3.75313 10000.000 10000.000
102 1018.1677 8.26403 4.45411 3.77090 10000.000 10000.000
103 1029.7042 8.30409 4.47593 3.78131 10000.000 10000.000
104 1041.2407 8.37659 4.51706 3.79888 10000.000 10000.000
105 1052.7650 8.41627 4.53877 3.80921 10000.000 10000.000
106 1064.2843 8.48861 4.58007 3.82678 10000.000 10000.000
107 1075.8035 8.52834 4.60191 3.83709 10000.000 10000.000
108 1087.3227 8.60152 4.64392 3.85485 10000.000 10000.000
109 1104.0000 8.67582 4.68675 3.87285 10000.000 10000.000
110 1104.0000 9.19535 4.96725 3.97973 10000.000 10000.000
111 1121.8813 9.20577 4.97087 3.98282 10000.000 10000.000
112 1133.4005 9.21966 4.97658 3.98647 10000.000 10000.000
113 1144.9128 9.24063 4.98699 3.99154 10000.000 10000.000
114 1156.3966 9.26162 4.99758 3.99670 10000.000 10000.000
115 1167.8803 9.27617 5.00395 4.00056 10000.000 10000.000
116 1179.3641 9.29717 5.01480 4.00584 10000.000 10000.000
117 1190.8478 9.31143 5.02116 4.00972 10000.000 10000.000
118 1202.3316 9.33251 5.03237 4.01515 10000.000 10000.000
119 1213.8153 9.34692 5.03900 4.01913 10000.000 10000.000
120 1225.2991 9.36812 5.05063 4.02474 10000.000 10000.000
121 1236.7559 9.38939 5.06252 4.03047 10000.000 10000.000
122 1248.1884 9.40371 5.06942 4.03458 10000.000 10000.000
123 1259.6210 9.42516 5.08183 4.04054 10000.000 10000.000
124 1271.0536 9.43953 5.08902 4.04477 10000.000 10000.000
125 1282.4862 9.46109 5.10192 4.05095 10000.000 10000.000
126 1293.9196 9.47543 5.10933 4.05529 10000.000 10000.000
127 1305.3522 9.49737 5.12299 4.06179 10000.000 10000.000
128 1316.7350 9.51961 5.13720 4.06854 10000.000 10000.000
129 1328.1029 9.53408 5.14523 4.07315 10000.000 10000.000
130 1339.4708 9.55660 5.16021 4.08023 10000.000 10000.000
131 1350.8387 9.57108 5.16857 4.08500 10000.000 10000.000
132 1362.2066 9.59420 5.18469 4.09258 10000.000 10000.000
133 1373.5745 9.61735 5.20125 4.10037 10000.000 10000.000
134 1384.8738 9.63212 5.21053 4.10554 10000.000 10000.000
135 1396.1715 9.65276 5.22546 4.11094 10000.000 10000.000
136 1407.4692 9.65897 5.22707 4.11518 10000.000 10000.000
137 1418.7669 9.66480 5.22834 4.11742 10000.000 10000.000
138 1430.0519 9.67061 5.22960 4.11966 10000.000 10000.000
139 1441.2813 9.67641 5.23085 4.12189 10000.000 10000.000
140 1452.5107 9.68218 5.23209 4.12411 10000.000 10000.000
141 1463.7400 9.68794 5.23332 4.12633 10000.000 10000.000
142 1474.9461 9.69366 5.23454 4.12855 10000.000 10000.000
143 1486.1144 9.69939 5.23575 4.13076 10000.000 10000.000
144 1497.2827 9.70508 5.23695 4.13297 10000.000 10000.000
145 1508.4240 9.71077 5.23814 4.13517 10000.000 10000.000
146 1519.5446 9.71643 5.23933 4.13736 10000.000 10000.000
147 1530.6440 9.72207 5.24050 4.13955 10000.000 10000.000
148 1541.7218 9.72770 5.24166 4.14174 10000.000 10000.000
149 1547.1716 9.73330 5.24282 4.14392 10000.000 10000.000
150 1547.1716 6.50000 0.02000 6.06900 10000.000 10000.000
#------------------------------------------------------------------------------
#
# LAYERED EARTH MODEL
# (ONLY THE SHALLOW RECEIVER STRUCTURE)
# =====================================
# 1. number of data lines of the layered model
#
# Note: if the number = 0, then the receiver site is the same as the
# source site, else different receiver-site structure is considered.
# please be sure that the lowest interface of the receiver-site
# structure given given below can be found within the source-site
# structure, too.
#
#------------------------------------------------------------------------------
0 |int: no_model_lines;
#------------------------------------------------------------------------------
#
# MULTILAYERED MODEL PARAMETERS (shallow receiver-site structure)
# ===============================================================
# no depth[km] vp[km/s] vs[km/s] ro[g/cm^3] qp qs
#------------------------------------------------------------------------------
1 0.000 2.900 1.676 2.600 92.00 41.00
2 2.000 2.900 1.676 2.600 92.00 41.00
3 2.000 5.400 3.121 2.600 92.00 41.00
4 7.000 5.400 3.121 2.600 92.00 41.00
5 7.000 6.160 3.561 2.600 576.00 256.00
6 17.000 6.160 3.561 2.600 576.00 256.00
7 17.000 6.630 3.832 2.900 576.00 256.00
8 35.000 6.630 3.832 2.900 576.00 256.00
9 35.000 8.0400 4.4700 3.3198 1340.00 600.00
#---------------------------------end of all inputs----------------------------
Note 1:
The slowness is defined by inverse value of apparent wave velocity = sin(i)/v
with i = incident angle and v = true wave velocity.
Note 2:
The suppression of the time domain aliasing is achieved by using the complex
frequency technique. The suppression factor should be a value between 0 and 1.
If this factor is set to 0.1, for example, the aliasing phase at the reduced
time begin is suppressed to 10%.
Note 3:
The default basic wavelet function (option 1) is (2/tau)*sin^2(pi*t/tau),
for 0 < t < tau, simulating physical delta impuls. Its half-amplitude cut-off
frequency is 1/tau. To avoid high-frequency noise, tau should not be smaller
than 4-5 time samples.
Note 4:
Double-Couple m11/ m22/ m33/ m12/ m23/ m31 Azimuth_Factor_(tz,tr,tv)/(tt)
============================================================================
explosion 1.0/ 1.0/ 1.0/ -- / -- / -- 1.0 / 0.0
strike-slip -- / -- / -- / 1.0/ -- / -- sin(2*azi) / cos(2*azi)
1.0/-1.0/ -- / -- / -- / -- cos(2*azi) / -sin(2*azi)
dip-slip -- / -- / -- / -- / -- / 1.0 cos(azi) / sin(azi)
-- / -- / -- / -- / 1.0/ -- sin(azi) / -cos(azi)
clvd -0.5/-0.5/ 1.0/ -- / -- / -- 1.0 / 0.0
============================================================================
Single-Force fx / fy / fz Azimuth_Factor_(tz,tr,tv)/(tt)
============================================================================
fz -- / -- / 1.0 1.0 / 0.0
fx 1.0/ -- / -- cos(azi) / sin(azi)
fy -- / 1.0/ -- sin(azi) / -cos(azi)
============================================================================
Note 5:
Layers with a constant gradient will be discretized with a number of homogeneous
sublayers. The gradient resolutions are then used to determine the maximum
allowed thickness of the sublayers. If the resolutions of Vp, Vs and Rho
(density) require different thicknesses, the smallest is first chosen. If this
is even smaller than 1% of the characteristic wavelength, then the latter is
taken finally for the sublayer thickness.