Appendix Ia
Seismogenic Sources - from Geologic/Geophysical Data
This category contains seismogenic sources for which either geological or geophysical evidence is available. See § 2.2.3.1. for a detailed explanation of all parameters used to describe these sources and § 3.3.2.1. to learn how to visualise them within the computer version of the Database. Notice that sources of this category were assigned an ID ranging from 1 to 200.
|
ID Source |
Source Name |
Quality |
Evidence |
Compiler(s) |
Length |
Width |
Strike |
Dip |
Rake |
Min dep |
Max dep |
|
1 |
Ovindoli-Pezza |
B |
Geological and geomorphological observations of surface faulting |
P. Burrato |
27.0 |
15.0 |
151 |
60 |
270 |
1.0 |
14.0 |
|
2 |
Fucino Basin |
A |
Geological observations of coseismic surface faulting and analytical modelling of coseismic elevation changes |
P. Burrato |
28.0 |
15.4 |
145 |
60 |
270 |
1.0 |
14.3 |
|
3 |
Aremogna-Cinque Miglia |
B |
Geomorphological and paleoseismological observations of surface faulting |
P. Bordoni and D. Pantosti |
20.0 |
12.2 |
144 |
60 |
270 |
1.0 |
11.6 |
|
4 |
Boiano Basin |
B |
Geomorphological features, surface and subsurface geological observations (analytical modelling) |
G. Valensise |
24.0 |
13.8 |
304 |
55 |
270 |
1.0 |
12.3 |
|
5 |
Tammaro Basin |
C |
Historical reports of damage, geomorphic evidence and extrapolation from neighbouring faults |
P. Bordoni and D. Pantosti |
25.0 |
14.3 |
311 |
60 |
270 |
1.0 |
13.4 |
|
6 |
Ufita Valley |
C |
Historical reports of damage, geomorphic evidence and extrapolation from neighbouring faults |
P. Bordoni and D. Pantosti |
26.0 |
14.7 |
308 |
60 |
270 |
1.0 |
13.7 |
|
7 |
Irpinia South |
A |
Seismological and geodetic observations, geological observations of coseismic surface faulting |
P. Burrato |
38.0 |
15.0 |
310 |
60 |
270 |
1.0 |
14.0 |
|
8 |
Agri Valley |
B |
Geomorphological features and geological observations (analytical modelling) |
P. Burrato |
23.0 |
13.5 |
316 |
60 |
270 |
1.0 |
12.7 |
|
9 |
Castrovillari |
B |
Geological and geomorphological observations of surface faulting |
P. Burrato |
15.6 |
10.3 |
158 |
60 |
270 |
1.0 |
9.9 |
|
10 |
Melandro-Pergola |
C |
Geomorphological features, topographic anomalies and constraints from extrapolation from neighbouring faults |
P. Burrato and G. Valensise |
17.9 |
11.3 |
317 |
60 |
270 |
1.0 |
10.8 |
|
11 |
Upper Mesima Basin |
C |
Historical reports of damage, geomorphic observations and extrapolation from neighbouring faults |
P. Burrato and G. Valensise |
22.0 |
13.5 |
30 |
30 |
270 |
3.0 |
9.8 |
|
12 |
Gioia Tauro Plain |
C |
Geomorphological features and geological observations (analytical modelling) |
P. Burrato and G. Valensise |
25.0 |
15.0 |
30 |
30 |
270 |
3.0 |
10.5 |
|
13 |
Messina Straits |
B |
Geodetic and geological observations. Analytical modelling of coseismic elevation changes and long-term geomorphology |
P. Burrato |
31.4 |
15.0 |
30 |
29 |
270 |
3.0 |
10.2 |
|
14 |
Belice |
B |
Seismological observations constrained by geomorphic evidence and damage pattern |
G. D'Addezio and G. Valensise |
11.0 |
6.5 |
277 |
55 |
127 |
3.0 |
8.3 |
|
15 |
Montereale Basin |
C |
Historical reports of coseismic ruptures and damage distribution constrained by regional tectonics |
P. Bordoni and R. Basili |
23.4 |
13.6 |
147 |
60 |
270 |
1.0 |
12.8 |
|
16 |
Norcia Basin |
C |
Historical reports of coseismic ruptures and damage distribution constrained by regional tectonics |
P. Bordoni |
25.0 |
14.3 |
157 |
60 |
270 |
1.0 |
13.4 |
|
17 |
Colfiorito North |
A |
Seismological and geodetic data |
R. Basili |
12.0 |
7.5 |
152 |
40 |
280 |
4.0 |
8.8 |
|
18 |
Colfiorito South |
A |
Seismological and geodetic data |
R. Basili |
9.0 |
6.0 |
148 |
40 |
277 |
4.0 |
7.8 |
|
19 |
Sellano |
A |
Seismological and geodetic data and observations of coseismic surface ruptures |
R. Basili |
6.0 |
6.0 |
144 |
40 |
260 |
2.5 |
6.5 |
|
20 |
Monte Sant'Angelo |
C |
Geomorphic and geologic observations |
D. Pantosti and L. Piccardi |
20.0 |
12.0 |
280 |
80 |
215 |
0.0 |
11.8 |
|
21 |
San Giovanni Rotondo |
C |
Geomorphic and geologic observations |
D. Pantosti, G. Valensise and L. Piccardi |
11.0 |
12.0 |
85 |
80 |
215 |
0.0 |
11.8 |
|
22 |
San Marco Lamis |
C |
Geomorphic, geologic, and seismological observations |
D. Pantosti, G. Valensise and L. Piccardi |
10.0 |
12.0 |
95 |
80 |
215 |
0.0 |
11.8 |
|
23 |
Mercure Basin |
C |
Tilting of recent lake deposits associated with migration of basin depocenter plus microtectonic constrains |
P. M. De Martini |
22.0 |
12.7 |
335 |
60 |
270 |
1.0 |
12.0 |
|
25 |
Campotosto |
C |
Geological observations of bedrock fault-scarps |
R. Basili |
14.0 |
9.5 |
150 |
65 |
270 |
1.0 |
9.6 |
|
26 |
Amatrice |
C |
Geological observations of bedrock fault-scarps |
R. Basili |
14.0 |
9.5 |
150 |
65 |
270 |
1.0 |
9.6 |
|
27 |
Sulmona Basin |
C |
Geological observations of bedrock fault-scarps |
R. Basili |
20.0 |
12.2 |
135 |
60 |
270 |
1.0 |
11.6 |
|
28 |
Barrea |
B |
Seismological observations constrained by intensity data and structural evidence |
P. Vannoli and R. Basili |
10.0 |
7.5 |
152 |
50 |
264 |
5.0 |
10.7 |
|
29 |
Conero offshore |
D |
Intensity data constrained by extrapolation from neighbouring faults |
R. Basili |
6.1 |
5.5 |
132 |
33 |
90 |
3.0 |
6.0 |
|
30 |
Senigallia |
C |
Subsurface geology constrained by geomorphic observations and intensity data |
R. Basili |
12.0 |
6.0 |
132 |
30 |
90 |
3.0 |
7.0 |
|
31 |
Fano Ardizio |
C |
Subsurface geology constrained by geomorphic observations and intensity data |
R. Basili and G. Valensise |
12.0 |
8.0 |
132 |
30 |
90 |
3.0 |
7.0 |
|
32 |
Pesaro San Bartolo |
C |
Subsurface geology constrained by geomorphic observations and intensity data |
R. Basili and G. Valensise |
8.0 |
6.0 |
122 |
30 |
90 |
3.0 |
6.0 |
|
33 |
Rimini offshore South |
D |
Subsurface geology constrained by geomorphic observations and intensity data |
R. Basili and G. Valensise |
8.0 |
5.0 |
132 |
30 |
90 |
3.0 |
5.5 |
|
34 |
Rimini offshore North |
D |
Subsurface geology constrained by geomorphic observations and intensity data |
R. Basili and G. Valensise |
8.0 |
5.0 |
132 |
30 |
90 |
3.0 |
5.5 |
|
35 |
Rimini |
C |
Subsurface geology constrained by geomorphic observations and intensity data |
R. Basili and G. Valensise |
8.0 |
6.0 |
132 |
30 |
90 |
3.0 |
6.0 |
|
36 |
Val Marecchia |
C |
Subsurface geology constrained by geomorphic observations and intensity data |
R. Basili and G. Valensise |
9.0 |
6.0 |
132 |
30 |
90 |
3.0 |
6.0 |
|
37 |
Gubbio South |
B |
Seismological observations constrained by subsurface geology and location of transverse lineaments |
S. Pucci |
7.5 |
4.0 |
140 |
21 |
270 |
4.6 |
6.0 |
|
38 |
Gubbio Middle |
C |
Seismological observations constrained by subsurface geology, continuity of regional trend and extrapolation from neighbouring faults |
S. Pucci |
7.5 |
4.0 |
140 |
15 |
270 |
3.5 |
4.5 |
|
39 |
Gubbio North |
D |
Constrained by subsurface geology, continuity of regional trend and extrapolation from neighbouring faults |
S. Pucci |
7.5 |
4.0 |
140 |
21 |
270 |
3.6 |
5.0 |
|
40 |
Aspromonte Northwest |
C |
Historical reports of damage constrained by geomorphic observations and regional geodynamics |
G. Valensise and P. Burrato |
5.0 |
4.5 |
300 |
70 |
225 |
3.0 |
7.2 |
|
41 |
Scilla offshore |
D |
Historical reports of damage constrained by geomorphic observations and regional geodynamics |
G. Valensise and P. Burrato |
5.0 |
4.5 |
300 |
70 |
225 |
3.0 |
7.2 |
|
42 |
Aspromonte Northeast |
C |
Historical reports of damage constrained by geomorphic observations and regional geodynamics |
G. Valensise and P. Burrato |
10.0 |
7.5 |
300 |
70 |
225 |
3.0 |
10.0 |
|
43 |
Aspromonte East |
C |
Historical reports of damage constrained by geomorphic observations, regional geodynamics |
G. Valensise and P. Burrato |
12.5 |
8.8 |
300 |
70 |
225 |
3.0 |
11.3 |
|
44 |
Nicotera-Rosarno |
C |
Historical reports of damage constrained by geomorphic observations and regional geodynamics |
G. Valensise and P. Burrato |
12.5 |
8.8 |
120 |
70 |
315 |
3.0 |
11.3 |
|
50 |
Garfagnana North |
B |
Intensity data constrained by regional geodynamics, geomorphic observations and location of transverse lineaments |
G. Vannucci and G. Valensise |
18.0 |
11.3 |
305 |
40 |
270 |
1.0 |
8.3 |
|
51 |
Garfagnana South |
C |
Geomorphic observations constrained by regional geodynamics and location of transverse lineaments |
G. Vannucci and G. Valensise |
15.0 |
10.0 |
307 |
40 |
270 |
1.0 |
7.4 |
|
100 |
Bagnacavallo |
C |
Intensity data constrained by geomorphic (river diversions) and geophysical exploration observations |
P. Burrato and G. Valensise |
10.0 |
6.0 |
119 |
30 |
90 |
3.0 |
6.0 |
|
101 |
Montello |
C |
Geomorphological features (river diversion and modelling of fluvial terraces) constrained by geophysical exploration observations depth |
P. Burrato and G. Valensise |
15.0 |
8.0 |
234 |
30 |
90 |
2.0 |
6.0 |
|
102 |
Asolo |
C |
Intensity data constrained by regional tectonics |
P. Burrato |
27.0 |
9.0 |
149 |
80 |
170 |
1.0 |
9.9 |
|
103 |
Mantova |
C |
Geomorphological features (river diversion) and topographic anomalies constrained by repeated levelling |
P. Burrato and G. Valensise |
10.0 |
6.0 |
262 |
30 |
90 |
3.0 |
6.0 |
|
104 |
Orzinuovi |
C |
Geomorphic evidence (river diversion and behaviour) and geophysical exploration observations supported by intensity data |
P. Burrato and G. Valensise |
10.0 |
6.0 |
266 |
30 |
90 |
2.0 |
5.0 |
|
105 |
Adige Plain |
C |
Geomorphological features (river diversion) and topographic anomalies |
P. Burrato and G. Valensise |
15.0 |
8.5 |
255 |
30 |
90 |
3.0 |
7.3 |
|
107 |
Mirandola |
C |
Subsurface geology constrained by geomorphic observations |
P. Burrato and G. Valensise |
12.0 |
10.0 |
115 |
30 |
90 |
3.0 |
8.0 |
|
120 |
Gemona East |
A |
Seismological observations constrained by geodetic and intensity data |
E. Baroux and P. Burrato |
16.0 |
12.0 |
270 |
20 |
90 |
2.0 |
6.1 |
|
121 |
Gemona North |
B |
Seismological observations constrained by geodetic and intensity data |
E. Baroux and P. Burrato |
8.0 |
6.0 |
230 |
60 |
46 |
1.0 |
6.2 |
|
122 |
Gemona West |
B |
Seismological observations constrained by geodetic and intensity data |
E. Baroux and P. Burrato |
8.5 |
7.0 |
270 |
30 |
90 |
6.5 |
10.0 |
|
123 |
Pordenone North |
C |
Extrapolation from neighbouring faults and regional tectonics |
P. Burrato and G. Valensise |
8.0 |
5.5 |
215 |
30 |
80 |
2.0 |
4.8 |
|
124 |
Cansiglio |
B |
Seismological, subsurface geology and intensity data |
P. Burrato and G. Valensise |
12.0 |
7.3 |
230 |
50 |
64 |
1.0 |
6.6 |
|
125 |
Alpago |
C |
Intensity data constrained by regional tectonics |
P. Burrato and G. Valensise |
18.0 |
9.0 |
206 |
55 |
50 |
1.0 |
8.4 |
|
126 |
Cividale |
C |
Distribution of intensity data points and surface geology |
P. Burrato |
25.0 |
9.3 |
313 |
70 |
180 |
1.3 |
10.0 |
|
130 |
Imperia |
C |
Intensity data constrained by tsunami evidence and regional geodynamics |
G. Valensise |
20.3 |
10.6 |
259 |
30 |
90 |
3.0 |
8.3 |