Andrea Spinelli and Gianluca Valensise
This chapter describes the structure of the GIS
that governs the Database of Potential Sources for Earthquakes Larger
than M 5.5 in Italy. In particular, section 2.1. provides a quick overlook
of the entire software, of the relational structure, of the layer structure
and of the main functions. The full detail on individual functions and
on how to operate with them during a working session is given in section
3.2. Section 2.2. describes the complete architecture of the system, with
a detailed description of the different table types and of the internal
structure of the tables that are most likely to be updated or extended
by individual future users of the Database.
This section provides a quick overview of the
Database of Potential Sources for Earthquakes Larger than M 5.5 in Italy.
This overview is especially recommended for first-time users that want
to learn quickly about the main features of the Database and the
essential operating requirements.
2.1.1. Operations Concept
The Database of Potential Sources for Earthquakes
Larger than M 5.5 in Italy is a tool that enables geologists, geophysicists,
earthquake and planning engineers to access detailed information about
known Italian seismogenic sources, as well as a comprehensive set of background
information, including administrative, geographical and earthquake data.
The user is encouraged to refer to Chapter 1 for the definition of seismic
source and of other conventional names used throughout this manual.
The Database may also be used as a tool for civil defence purposes
as it can generate first-level damage scenarios for an imaginary earthquake
of given location and magnitude.On startup the user is presented with a
map the main topographic features of Italy shown through a Digital Elevation
Model. The map can be manipulated using some of the standard Geographic
Information Systems (GIS) tools (e.g., zooming, panning, distance measurement,
changing coordinate system, etc.). The user may superimpose on this basic
map a set of layers which can be roughly classified into the three following
categories:
2.1.2. Application Category
The Database is a MapInfo®
application; as such, it is compiled in a neutral, proprietary format
which can be executed on several platforms, including Microsoft Windows
9x/NT/2000 and MacOs. We did not test the Database on a Unix platform.
The application is standalone and access to data is essentially read-only.
Therefore, multiple users in the same organisation must copy the database
on as many workstations as required.
The Database is distributed on a single
ISO 9660 CD, which may be accessed both by Windows and Macintosh computers.
It requires installation of a properly working copy of MapInfo®
4.0 or higher version; MapInfo® is not
included in the distribution.
2.1.3. Relational Structure
All data are stored in MapInfo®
structures (tables); according to the content, they may be classified as
relational
tables and raster tables. Relational tables contain alphanumerical
and geographical information; raster tables simply provide georeferencing
for a bitmap (graphics data file). The total number of individual tables
used by the system is over 650. In the rest of this section we discuss
the Entity-Relationship model of the relational tables. Subsequent sections
of the manual will describe relational and raster tables from a more application-oriented
viewpoint.From a relational perspective, we decided to de-normalise
several tables describing seismic sources, namely SourceDeep, SourceGeol,
SourceHistA, SourceHistARev, SourceHistB, SourceHistBRev, SourceInferred
and SourcePreferred. However, all of those tables share a single
object identity pool, and may therefore be considered as a single Source
table in E-R diagrams.
The first E-R diagram shows the central role of the Seismic Source
concept in the Database.

An essential piece of information contained in
the Database is given by earthquake catalogues of historical and
instrumental seismicity and by the individual intensity reports associated
with historical events. The Database contains one instrumental catalogue
(the INGV official catalogue, stored as
Inst_q.tab:
see § 2.2.5.2.1. for further details), plus three historical catalogues,
whose acronyms are CFTI 3, NT 4.1.1 and CPTI (stored as
CFTI_q.tab,
NT_q.tab,
CPTI_q.tab,
respectively: see § 2.2.5.2.2.). CFTI 3 and NT 4.1.1 have felt intensity
reports associated with them, while CPTI and the INGV instrumental database
have a flatter structure.

The rest of the database consist of flat tables,
reflecting the co-existence of data coming from diverse sources that are
integrated only by their geographic superposition. They lack any relational
structure and are not presented here, although they will be discussed in
detail in subsequent sections. However, there is a pattern of relationship
among tables which is not reflected in the classic E-R theory, but deserves
some explanation: it is formed by a table which is a catalogue of layers
to be shown or hidden at the user's request. For each collection, only
one layer of the collection is displayed at any one time; some additional
data may also be available in alphanumeric form. The following figure documents
the occurrences of this pattern.

2.1.4. Layer Structure
The following table indicates the physical order
in which layers are shown and provides a brief description for each layer.
The user may refer to the following sections for a more thorough explanation
of structures and scopes.
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Cosmetic layer (INGV logo, decorations, …) |
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Scale |
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Fault scarps |
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Seismogenic Sources |
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" |
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" |
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" |
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" |
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" |
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" |
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" |
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Tectonic lineaments |
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Tectonic lineaments |
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Currently-open additional data |
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Labels for intensities (earthquake catalogues with felt maps) |
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Additional info for felt reports |
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Locality names |
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" |
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" |
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Instrumental earthquakes from the INGV catalogue |
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Historical earthquakes from CFTI 3 catalogue |
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Historical earthquakes from CPTI catalogue |
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Historical earthquakes from NT 4.1.1 catalogue |
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Administrative boundaries for the Italian "Comuni" |
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Administrative boundaries for the Italian "Provincie" |
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Administrative boundaries for the Italian "Regioni" |
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Grids at several spacings |
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Main rivers |
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Main lakes |
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Intermediate-scale drainage countrywide |
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Small-scale drainage for the Italian "Regioni" |
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Currently open fault compilation |
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Coastline for European-Mediterranean countries, except Italy |
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Coastline for European-Mediterranean countries and Italy |
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Several layers of bathymetry in Black and White |
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Several layers of bathymetry, Colour Coded |
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Tiles of the Colour Coded DEM |
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Tiles of the Shaded Relief DEM |
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Tiles of the Black and White DEM |
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Empty layer; used as a sentinel value |
2.1.5. Functions
The main function classes of the application may be grouped in several broad categories, which are reflected in the application menus:
a. allows the user to print or save the currently open table or map, exit MapInfo ® altogether, or close the DISS application, leaving open all the relevant tables. This feature allows for further elaboration of available data;
b. allows the user to show or hide some of the main available data layers; the application maintains a layer ordering which is meant to maximise data visibility;
c. makes the usual GIS operators available to the user and allows the standard operations of zooming, panning, distance measuring, selecting objects, selecting a new coordinate system, etc.;
d. when a seismic source has been selected, it gives access to its relational information through a series of specifically designed dialog boxes;
e. gives access to a similar but smaller set of dialog boxes showing information about tectonic lineaments;
f. allows a concerned user (for example, a civil defence officer) to simulate earthquake intensities and estimate the earthquake impact on urban nuclei, obtaining reports both in tabular and geographic format;
g. allows a system engineer to perform
maintenance operations to enter new or updated information in the
Database.
This section describes how the Database is organised, how the different tables interact with each other to make it work, and the current content of its non-structural part (see description of table types in § 2.2.2.). To improve readability the text will make use of the following typing conventions all throughout:
- Courier Boldface will be used for all physical table and folder names;
- Courier Plain Text will be used for the name and format of the fields forming a table;
- Palatino Italic will be used for menu names and virtual table names;
- Palatino Plain Text will be used for all the rest, except for recurring names such as "Database" and for sentences that require special emphasis.
2.2.1. Directory Structure
The directory structure of the software reflects
as much as possible the categorisation of data in the user domain. The
MapInfo® compiled program, DISS.mbx, is located
in the main directory of the product along with the three main subdirectories
that contain all the Database information. The subdirectories contain
the data layers, according to the following scheme:
| Directory name | Description |
| Background_Info | Support tables |
| Background_Info/Administrative | Administrative data |
| Background_Info/DEM | Digital Elevation Model |
| Background_Info/DEM/Bathymetry | Bathymetry of Mediterranean |
| Background_Info/DEM/BW | Black and white DEM |
| Background_Info/DEM/ColourCoded | Colour coded DEM |
| Background_Info/DEM/ShadedRelief | Shaded relief DEM |
| Background_Info/Geographic | Rivers, lakes, coastlines |
| Background_Info/Geological | Geological data |
| Background_Info/Geological/Additional_Data | Additional data (catalogue of) |
| Background_Info/Geological/Compilations | Fault compilations (catalogue of) |
| Background_Info/Geological/Compilations/Maps | Individual fault compilations |
| Background_Info/Grids | Geographic grid (variable spacing) |
| Background_Info/Seismicity | Earthquake catalogues |
| Source_Data | Specific information about sources |
| Source_Literature | Published info about specific sources |
| Source_Literature/Open_Questions | Comments and open questions |
| Source_Literature/Pictures | Pictures about faults |
| Source_Literature/Previous_Studies | Summaries of Previous Studies |
2.2.2. Table types
The Database contains three main categories of tables:
Structural tables contain the core of the
Database, that is, the seismogenic sources. They include the geographic
representation of each source along with all the related alphanumeric information.
The structure and the content of these tables are illustrated in §
2.2.3.
Instrumental tables are used to relate
to each source all the information available on it, such as references,
pictures and text summaries. The structure and the content of these tables
are illustrated in § 2.2.4.
Support tables contain several types of
data to support the consultation of the Database and help placing
the seismogenic sources in their actual seismological, geographic and administrative
context. Support tables may be source-specific,
source-generic,
or generic. The structure and the content of these tables are illustrated
in § 2.2.5.
| Table type | Located in folder |
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| Structural Tables | Source_Data |
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| Instrumental Tables | Source_Data |
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| Support
Tables:
- Source-generic - Generic |
Source_Literature
BackGround_Info > Geological BackGround_Info > (all others) |
§ 2.2.5.2. § 2.2.5.3. |
All tables have (1) a standard or virtual name
that refers to their actual content and to the corresponding menu item,
and (2) a physical name used to identify the relevant file(s) in the disk
database. The menu item name was selected to allow easy identification
of the scope and information content of a specific table and is normally
formed by a sequence of words in "title case" (all initials are written
in uppercase, e.g.: Seismogenic Sources from Geologic/Geophysical Data).
The physical table filename uses the same keywords in a condensed form
and with optional underscore ("_") symbols in place of blank spaces (e.g.
Seismogenic Sources from Geologic/Geophysical Data " SourceGeol.tab).
All filenames are subject to restrictions imposed by MapInfo® and were
selected following the naming conventions of Apple OS and Windows 95 and
higher.
In the following we will describe the general
structure of all the tables used by the Database. A detailed description
of the internal structure and of individual data fields is supplied for
those tables that can be more easily updated or extended by the user. The
internal structure of each table can also be explored directly using MapInfo®
through the menu sequence
Table > Maintenance > Table Structure.
2.2.3. Structural Tables
All the seismogenic sources contained in the Database are organised in six main categories, depending on how they were derived and on the overall reliability of their identification and characterisation:
2.2.3.1. Seismogenic Sources from Geologic/Geophysical Data
This category stores data on seismogenic sources for which either geological or geophysical evidence is available and that received special attention during the compilation of the Database. For all sources of this group the compiler has brought together geological, seismological and other geophysical information (essentially references and pictures) and has prepared Summaries of the Main Studies on the Source and Comments and Open Questions files. The name of the associated physical table is SourceGeol.tab.
Table structure:
SourceGeol.tab
| Field name | Content | Format |
| SourceName | Encodes the source by a name | Char(50) |
| IDSource | Encodes the source by an identification number. Ranges between 1-200 for Geologic/Geophysical sources | Integer |
| Quality | Reliability of source data. See text for details | Char(1) |
| lat1
lon1 lat2 lon2 lat3 lon3 lat4 lon4 |
Geographic
coordinates of the corners of the box representing the surface projection
of the source. The corners are numbered conventionally starting from the
northernmost upper one and moving in the clockwise or anticlockwise direction
respectively for a W- or E- dipping plane. Note that corners 1 and 2 are
always associated with the upper edge of the box
|
Char(8)
Char(8) Char(8) Char(8) Char(8) Char(8) Char(8) Char(8) |
| Length | Length of segment joining the two uppermost tips of the fault plane (km) | Char(8) |
| Width | Down-dip width of the fault plane, that is, the length of the segment traced between the top and the bottom of the fault plane (km) | Char(4) |
| Strike | Strike is measured in degrees clockwise with respect to the North using the following convention: E-dipping planes strike between 270° and 90°; W-dipping planes strike between 90° and 270° | Char(10) |
| Dip | Angle between the fault plane and the horizontal (degrees) | Char(4) |
| Rake | Expresses the sense of motion of the hanging-wall with respect to the foot-wall and is measured counterclockwise (degrees) starting from the horizontal. The rake of a pure normal, reverse, left-lateral and right-lateral fault is 270°, 90°, 0° and 180°, respectively | Char(4) |
| Min_Depth | Min depth of fault plane from topographic surface (km) | Char(8) |
| Max_Depth | Max depth of fault plane from topographic surface (km) | Char(8) |
| Evidence | Type of evidence used to identify the source | Char(254) |
| latN
lonN latS lonS |
Coordinates
of northern and southern tips of:
|
Char(8)
Char(8) Char(8) Char(8) |
| Compiled_by | Name(s) of the compiler(s) of the given source | Char(50) |
| Preferred | States with a logical character (T/F, true/false) if the source should or should not be added to the Integrated Source Dataset | Logical |
Notice that the minimum depth of the fault plane from topographic surface must be intended as the depth of the seismogenic portion of the source. To avoid ambiguities and potential modelling problems, the minimum value for this parameter was conventionally set at 1 km. The underlying assumption is that the shallowest 1 km of crust above a seismogenic source may only react passively to slip on the underlying fault even if sizeable surface faulting may occur.
The rating of sources of this category through the field Quality is based on expert judgement by the compiler of each individual source. The process is very complex because of the large number and the diverse nature of uncertainty types involved in the identification and characterisation of any individual source. For example, some of the sources carry an epistemic uncertainty associated with their mere existence, or with their attitude towards generating their maximum-size earthquake versus releasing multiple smaller events. These types of non-conventional uncertainties are difficult to be incorporated into a single rating parameter and for the time being this task has been entirely left to the expert judgement of the individual compilers.
The following is a simplified scheme that was followed for rating all Geologic/Geophysical sources. Notice that additional information on the reliability of the proposed source parameters is generally contained in the Comments and Open Questions text associated with most sources.
Rating criteria: Geologic/Geophysical Sources
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Description |
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Class A is assigned to all sources for which there exists combined instrumental, historical and geologic/geomorphic evidence. The source parameters of Class A sources are constrained by seismological or geodetic evidence that allow a finer resolution than that granted by surface geology data alone. |
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Class B is assigned to all sources for which there exists satisfactory instrumental/historical/paleoseismological and geologic/geomorphic evidence. Class B typically includes the source of earthquakes that occurred in the pre-instrumental era. The source parameterisation is jointly constrained by the extent of the historical rupture and by the occurrence of significant geologic features such as the size and extent of a basin, the intersection with known tectonic lineaments, the rupture terminations of Class A sources, etc. |
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Class C is assigned to all sources that were derived from geologic/geomorphic evidence but for which limited or no historical evidence exists, or that possess satisfactory historical but limited/debatable geologic/geomorphic evidence. The source must be on-land and associated with clearly identified large-scale features belonging to known regional trends. This class and the following Class D also include sources for which there is epistemic uncertainty as to their existence as active features and to their potential as seismogenic sources. |
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Similarly to the rating C, Class D is assigned to all sources that were derived from geologic/geomorphic evidence with limited or no historical constraints. Unlike the previous class, the source may be offshore and its location constrained only by reflection seismology data or other large-scale observations used to pinpoint regional trends of homogeneous tectonic deformation. |
2.2.3.2. Seismogenic Sources - Historical - Well Constrained with Geological Background
Includes all seismogenic sources derived exclusively from intensity data following the method proposed by Gasperini et al. [1999] and for which the quality of the solution obtained was enough to allow the representation by an oriented rectangular box (see Figure 1 and relevant text in Gasperini et al. [1999]). For sources of this group the compiler has brought together support information (essentially references and pictures) and has prepared Summaries of the Main Studies on the Source and Comments and Open Questions files, similarly to what is done for all Sources from Geologic/Geophysical Data. The additional information, however, was not enough to allow the compiler to turn this source into a Geologic/Geophysical Source.
The name of the associated physical table is SourceHistARev.tab, where
| Field name | Content | Format |
| SourceName | Encodes the source by a name | Char(50) |
| IDSource | Encodes the source by an identification number. Ranges between 201-400 and 401-500 for sources without or with Geological Background, respectively | Integer |
| Quality | Reliability of source data expressed through two distinct parameters. See text for details | Char(3) |
| lat1
lon1 lat2 lon2 lat3 lon3 lat4 lon4 |
Geographic coordinates of the corners of the box representative of the source. The corners and the associated distances (Length, Width) are provided directly by the method proposed by Gasperini et al. [1999] | Char(8)
Char(8) Char(8) Char(8) Char(8) Char(8) Char(8) Char(8) |
| Length | Length of segment joining the two uppermost corners of the fault plane (km) | Char(8) |
| Width | Length of segment corresponding to a short side of the fault plane (km) | Char(4) |
| Strike | Strike is measured in degrees clockwise with respect to the North. Given the lack of information about the direction of dip of the fault, any strike value is equivalent to strike+180°. The uncertainty is supplied directly by the method proposed by Gasperini et al. [1999] | Char(10) |
| Evidence | Type of evidence used to identify the source | Char(254) |
| Compiled_by | Name(s) of the compiler(s) of the given source | Char(50) |
| Preferred | States with a logical character (T/F, true/false) if the source should or should not be added to the Integrated Source Dataset | Logical |
Notice that the structure of this table differs from that of SourceGeol.tab for the following reasons:
Rating criteria: all Historical Sources
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intensity data |
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2.2.3.3. Seismogenic Sources - Historical - Well Constrained, no Geological Background
Includes all seismogenic sources derived exclusively
from intensity data following the method proposed by Gasperini et al.
[1999] and for which the quality of the solution obtained was enough to
allow the representation by an oriented rectangular box (see Figure 1 and
relevant text in Gasperini et al. [1999]). For these sources, however,
no additional information is supplied by the compiler. The name of the
associated physical table is
SourceHistA.tab.
The structure of the table is the same as for
SourceHistARev.tab.
2.2.3.4. Seismogenic Sources - Historical - Poorly Constrained with Geological Background
Includes all seismogenic sources derived exclusively from intensity data following the method proposed by Gasperini et al. [1999] and for which the quality of the solution obtained was not enough to allow the representation by an oriented rectangular box (see Figure 1 and relevant text in Gasperini et al. [1999]). The source was then represented as a circle having the diameter equal to the estimated source length. For sources of this group the compiler has brought together support information (essentially references and pictures) and has prepared Summaries of the Main Studies on the Source and Comments and Open Questions files, similarly to what is done for the Geologic/Geophysical Sources. The additional information, however, was not enough to allow the compiler to turn this source into a Geologic/Geophysical Source.
The name of the associated physical table is SourceHistBRev.tab, where
| Field name | Content | Format |
| SourceName | Encodes the source by a name | Char(50) |
| IDSource | Encodes
the source by an identification number.
Ranges between 501-800 and 801-900 for sources without or with Geological Background, respectively |
Integer |
| Quality | Reliability of source data expressed through two distinct parameters. See text for details | Char(3) |
| lat
lon |
Centre of the circle representative of the source. The source radius is provided directly by the method proposed by Gasperini et al. [1999] | Char(8)
Char(8) |
| Radius | Radius of given source (km) | Char(8) |
| Evidence | Type of evidence used to identify the source | Char(254) |
| Compiled_by | Name(s) of the compiler(s) of the given source | Char(50) |
| Preferred | States with a logical variable (T/F, true/false) if the source should or should not be added to the Integrated Source Dataset | Logical |
Notice that the structure of this table differs from that of SourceHistARev.tab/ SourceHistA.tab for the following reasons:
For similarity with sources of the category Historical - Well Constrained, the field Quality contains two distinct parameters for assessing the uncertainties associated with the given source model. Notice that Q1 is always equal "E". See scheme at the end of § 2.2.3.2. for further details.
2.2.3.5. Seismogenic Sources - Historical
- Poorly Constrained, no Geological Background
Includes all seismogenic sources derived exclusively
from intensity data following the method proposed by
Gasperini et al.
[1999] and for which the quality of the solution obtained was not enough
to allow the representation by an oriented rectangular box (see Figure
1 and relevant text in Gasperini et al. [1999]). For these sources,
however, no additional information is supplied by the compiler. The name
of the associated physical table is
SourceHistB.tab.
The structure of the table is the same as for
SourceHistBRev.tab.
2.2.3.6. Deep
Includes sources derived exclusively from intensity data following the method proposed by Gasperini et al. [1999] and for which the compiler hypothesised a depth larger than ordinary (usually below 10 km). The assignment of a source to this category is irrespective of whether the formal uncertainties in the solution obtained would have allowed to derive a rectangular source or simply a circular source. Notice that in the case of a source deeper than usual the technique proposed by Gasperini et al. [1999] would not be able to derive correctly the true elongation of the source, and any asymmetries in the intensity pattern could more likely result from propagation effects.
The name of the associated physical table is SourceDeep.tab. To allow a better visual separation, sources of this category are drawn using hexagons.
Table structure: SourceDeep.tab
| Field name | Content | Format |
| SourceName | Encodes the source by a name | Char(50) |
| IDSource | Encodes
the source by an identification number.
Ranges between 901-1000 |
Integer |
| Quality | Reliability of source data expressed through two distinct parameters. See text for details | Char(3) |
| lat
lon |
Centre of the hexagon representative of the source. The source radius is provided directly by the method proposed by Gasperini et al. [1999] | Char(8)
Char(8) |
| Radius | Radius of given source (km) | Char(8) |
| Evidence | Type of evidence used to identify the source | Char(254) |
| Compiled_by | Name(s) of the compiler(s) of the given source | Char(50) |
| Preferred | States with a logical variable (T/F, true/false) if the source should or should not be added to the Integrated Source Dataset | Logical |
Notice that the structure of this table is virtually identical to that of SourceHistBRev.tab/SourceHistB.tab.
The field Quality
contains two distinct parameters for assessing the uncertainties associated
with the given source model. The assessment is done following the scheme
used for sources of the category Historical - Poorly Constrained.
Notice that Q1 is always equal "E". See scheme at the end of §
2.2.3.2. for further details.
2.2.3.7. Integrated Source Dataset
The structure of the
Database allows for
multiple solutions for the same physical seismogenic source. For example,
a source of the category Historical - Well Constrained will always
have also the corresponding solution in the category Historical - Poorly
Constrained and possibly also in the Geologic/Geophysical. The
Integrated Source Dataset (SourcePreferred.tab)
displays the "preferred" set of sources, that is to say, in case of multiple
solutions the compiler has made a decision concerning which source should
be used for further elaborations. The decision is made by setting the field
Preferred to "T" or "F" depending on whether the compiler
wants the specific source to be included or not included in the
Integrated
Source Dataset. Notice that this field appears in all primary structural
tables described in § 2.2.3. The Integrated Source Dataset
is generated by the Database itself during the
Maintenance
operations (see § 4.5.).
2.2.3.8. Seismic Behaviour
The table Seismic_Behaviour.tab stores parameters used to characterise the behaviour of each seismogenic source for all source categories. The table contains data selected or re-interpreted from published literature. If the information available is too complicated or controversial to be expressed by a number, the compiler fills-in the corresponding field with an asterisk and explains the matter in the Comments and Open Questions.
Table structure: Seismic_Behaviour.tab
| Field name | Content | Format |
| SourceName | Encodes the source by a name | Char(50) |
| IDSource | Encodes the source by an identification number | Integer |
| Last Earthquake | Date of most recent earthquake rupturing the entire length of the given seismogenic source | Char(150) |
| Prev Max Earthquake | List age of any previous maximum earthquakes identified from paleoseismological, geologic and historical evidence | Char(254) |
| Recurrence Interval | Average time span between two subsequent maximum events generated by the same source, expressed in years | Char(150) |
| Elapsed Time | Time elapsed since Last Earthquake, in years, conventionally referred to the year 2000 | Char(60) |
| Slip Rate | Slip-rate in mm/year, either published or estimated by the compiler based on original or published data. In either case, the section Comments and open questions should be used to explain how the slip-rate was estimated/computed | Char(254) |
| Average Displacement | Average coseismic displacement, in meters | Char(100) |
| Expected Magnitude | For Geologic/Geophysical
sources: magnitude calculated from source size through empirical relations.
For Historical sources: magnitude of historical earthquake (corresponding with magnitude used to assess source length and width) |
Char(100) |
2.2.3.9. Fault Scarps
The table FaultScarps.tab lists genuinely tectonic surface ruptures that are thought to slip in conjunction with one or more sources of the Geologic/Geophysical category. The ruptures are usually more than one and include primary ruptures located along the fault projection onto the surface and secondary ruptures located within the surface projection (e.g., in the hanging-wall compartment of a normal fault). Each rupture is identified by an IDScarp code and is logically linked to one or more individual sources through the IDSource code. However, this does not preclude that it may move as a result of the activation of other sources. Each rupture is characterised also by a name and bibliography references.
Notice that in the Database a surface rupture is intended as a strictly graphical object that is not described by geographic coordinates. This is due to the fact that some surface ruptures have a complex trend that may easily be described as a complex graphical object by the cartographic interface but that would be complicated to describe as a sequence of latitude-longitude pairs. The coordinates of each point of a given surface rupture can obviously be inferred from the cartographic interface using the standard tools of MapInfo®.
Table structure: FaultScarps.tab
| Field name | Content | Format |
| IDSource | Links the surface rupture with a seismogenic source | Integer |
| IDScarp | Encodes the rupture by a number. Further ruptures associated with the same source must have a different code | Integer |
| SourceName | Name of the source to which the surface rupture is linked | Char(32) |
| FaultScarpName | Encodes the surface rupture by a name | Char(60) |
| Reference | Reference(s) for the given surface rupture | Char(60) |
2.2.3.10. Tectonic Lineaments
The tables TransverseTectLineaments.tab and GenericTectLineaments.tab contain linear tectonic features taken from published literature. The first table contains lineaments that lie nearly perpendicular to the general trend of the main seismogenic sources, while all the remaining lineaments are included in the second table. These two subsets are prepared by the Database itself during the Maintenance operations starting from Tectonic_Lineaments.tab (see § 4.5.). Each lineament may be mapped as a single line or as a segmented element, depending on how it was originally drawn in the referenced paper(s). The Tectonic Lineaments may or may not be active or seismogenic; under special circumstances, limited portions of them may be identified as Geologic/Geophysical sources and treated accordingly. Similarly to the seismogenic sources, each Tectonic Lineament may be assigned one or more references (see § 2.2.4.4.).
Table structure:
Tectonic_Lineaments.tab
| Field name | Content | Format |
| Name | Encodes the tectonic lineament by the name with which it is identified in the referenced paper(s) | Char(50) |
| ID | Encodes the tectonic lineament by an identification number | Integer |
| Type | Describes the type of lineament as "G" (Generic) or "T" (Transverse) | Char(1) |
| Reliability | Rates the reliability of the given tectonic lineament on a scale of A (most reliable) to D (least reliable) | Char(16) |
| Evidence | Type of evidence available in literature to identify the given tectonic lineament | Char(80) |
| Notes | Describes the general geometry, kinematics and timing of the given tectonic lineament, with specific reference to the investigators that supplied the information | Char(250) |
2.2.3.11. Summary of structural tables
The following scheme summarises the correspondence
between standard and virtual names for all of the Structural Tables. "Corresponding
file(s)" specifies the location of the tables within the disk database.
The specification "Layer" indicates that the given table is also a layer
of the Geographic Information System, that is, has graphic objects associated
with it. These are drawn as specified in "Symbol" and with the colour specified
in "Colour".
| Table name/Menu item | Corresponding file(s) |
|
|
|
| Seismogenic Sources from Geologic/Geophysical Data | SourceGeol.tab
FaultScarps.tab |
|
|
Red |
| Seismogenic Sources - Historical -Well Constrained with Geological Background | SourceHistARev.tab |
|
|
|
| Seismogenic Sources - Historical -Well Constrained, no Geological Background | SourceHistA.tab |
|
|
|
| Seismogenic Sources - Historical -Poorly Constrained with Geological Background | SourceHistBRev.tab |
|
|
|
| Seismogenic Sources - Historical -Poorly Constrained, no Geological Background | SourceHistB.tab |
|
|
|
| Seismogenic Sources - Deep | SourceDeep.tab |
|
|
|
| Integrated Source Dataset | SourcePreferred.tab |
|
|
|
| Seismic Behaviour | Seismic_Behaviour.tab |
|
|
|
| Tectonic Lineaments | Tectonic_Lineaments.tab |
|
|
|
| Generic Tectonic Lineaments | GenericTectLineaments.tab |
|
|
|
| Transverse Tectonic Lineaments | TransverseTectLineaments.tab |
|
|
|
2.2.4. Instrumental Tables
These tables create logical links between each individual source and the information concerning it currently available in the Database. In particular these tables are used to assign to each source:
The table Assign_Studies.tab links each Summaries of the Main Studies on the Source text file with the seismogenic source to which it refers.
Table structure: Assign_Studies.tab
| Field name | Content | Format |
| IDSource | Encodes the source by an identification number | Integer |
| filename | Name of the file containing the Summaries of the Main Studies for the given source | Char(32) |
2.2.4.2. Assign Questions
The table Assign_Questions.tab links the Comments and Open Questions text file with the seismogenic source to which it refers.
Table structure:
Assign_Questions.tab
| Field name | Content | Format |
| IDSource | Encodes the source by an identification number | Integer |
| filename | Name of the file containing the Comments and Open Questions for the given source | Char(32) |
2.2.4.3. Assign Pictures
The table Assign_Pictures.tab stores data on images or photographs associated with a given source. More specifically, the table links each source with the titles and file names of the relevant pictures and of the associated captions.
Table structure: Assign_Pictures.tab
| Field name | Content | Format |
| IDSource | Links the picture to a source by its identification number | Integer |
| Title | Title of the picture as it will appear in the Pictures dialog box. The same title cannot be assigned to more than one picture within the same source | Char(50) |
| Picture | Name of the relational table associated with the raster file containing the picture | Char(32) |
| Caption | Name of the table containing the caption for the corresponding picture | Char(32) |
2.2.4.4. Assign References
The table Assign_References.tab lists in full detail all the references contained in the Database and links each of them to the seismogenic source or tectonic lineament to which it refers. More specifically, the table contains references:
Table structure: Assign_References.tab
| Field name | Content | Format |
| IDSource | Links to the relevant source or tectonic lineament by its identification number | Integer |
| Authors | Authors of given reference (see table for adopted format) | Char(249) |
| Year | Year of publication | Char(10) |
| Title | Full title of reference (see table for adopted format) | Char(254) |
| Reference | Full reference of journal, proceedings volume or book were the given paper was published. Journal titles should be abbreviated according to the World List of Abbreviations followed by volume number, first and last page (see table for adopted format) | Char(254) |
| Code_Year | Internal code (same as Year of publication) | Char(4) |
| Code_Language | Reference language: I=Italian, E=English, O=Other | Char(1) |
| Code_Publication | Reference type: A, B, J, M, P, V, W respectively for: Abstract, Book, Journal, Manuscript, Proceedings, Volume, Website (see § 2.2.4.4.2. for details) | Char(1) |
| Code_ReferenceID | Identification number of given reference within the Database printed paper files (see § 2.2.4.4.1. for details) | Char(4) |
| Availability | Y if paper is available in the Database printed paper files, otherwise N | Char(1) |
| TpLength
TpWidth |
Reference contains information on the length and width of the source (T or F) | Logical
Logical |
| TpStrike
TpDip TpRake |
Reference contains information on the strike, dip, and rake of the source (T or F) | Logical
Logical Logical |
| TpMinDepth
TpMaxDepth |
Reference contains information on the min, max depth of given source (T or F) | Logical
Logical |
| TpLastEq
TpMaxEq |
Reference contains information on the most recent earthquake and on the previous earthquake(s) generated by given source (T or F) | Logical
Logical |
| TpRecInt
TpElapTime |
Reference contains information on the recurrence interval and elapsed time for the given source (T or F) | Logical
Logical |
| TpSlipRate
TpAvDisp |
Reference contains information on the slip rate and average displacement for the given source (T or F) | Logical
Logical |
| TpExpMagn | Reference contains information on the magnitude of the largest earthquake expected to be generated by the given source (T or F) | Logical |
2.2.4.4.1. Assigning a new Code Reference
Any new reference is uniquely identified through
the Code_ReferenceID,
which is the code assigned to the given article, map, book or manuscript
within the physical database of printed papers available at Istituto Nazionale
di Geofisica e Vulcanologia in Rome. As explained in the chapter on Updating
the Database (§ 4.1.4.), it is suggested that the references table
be handled through a Microsoft® Excel twin copy
of Assign_References.tab.
This allows an easier check of the existing codes and a safer assignment
of a new one, which can simply be the next available four-digit number.
This number will appear printed on the paper stored in the physical database.
2.2.4.4.2. Filling-in the Code Publication field
This field is used to specify the type of publication that corresponds to each specific reference. Along with the Code_Language specifier, this field helps determining the characteristics of the papers that were used as a source of data for the compilation of the Database. The Code_ReferenceID and Availability specifiers help retrieving the publication of interest from the physical database of printed papers available at Istituto Nazionale di Geofisica e Vulcanologia in Rome.
Abstracts Includes all abstracts and posters presented at meetings or conferences regardless of whether the same material has subsequently been published on proceedings or on a journal.
Books Includes all books that are intended for commercial distribution and can be freely purchased from the publisher.
Journal Includes all articles that appear on peer-reviewed, regularly published journals, either national or international.
Manuscript Includes theses, internal reports and all other material that has not appeared in publication as such, which was not intended for distribution and that can only be obtained directly from the author.
Proceedings Includes conference proceedings that are part of a regular series of publications.
Volume Includes all publications that do not fall in any of the previous categories, e.g. conference proceedings that have been collected by one or more editors and are not part of a regular series, special celebration volumes, contributions to projects (only if available to the general public; otherwise they should be categorised as Manuscripts).
Website
Indicates that the information was obtained from a World Wide Web site,
regardless of whether the content of the site has been or will be published
in any other form.
2.2.4.5. Summary of instrumental tables
The following scheme summarises the correspondence
between standard and virtual names for all of the Instrumental Tables,
along with their links to folders and subfolders of the disk database.
| Table name/Menu item | Corresponding disk file(s) | Links to |
| Assign Studies | Assign_Studies.tab | Source_Literature
folder
Previous_Studies subfolder |
| Assign Questions | Assign_Questions.tab | Source_Literature
folder
Open_Questions subfolder |
| Assign Pictures | Assign_Pictures.tab | Source_Literature
folder
Pictures subfolder F* sub-subfolder |
| Assign References | Assign_References.tab | Physical database of printed papers at INGV, Rome |
2.2.5. Support Tables
These tables contain information that supports
many representation and operating functions. They are all accessed through
the menu View. The support information may be Source Specific,
Source Generic, or
Generic. Most of the information is public
domain or was derived from published datasets. The following description
is organised based on these three categories of Support Tables.
2.2.5.1. Source Specific support tables
These tables contain information that relates specifically to one of the sources. Notice that this type of information is available only for sources that belong to the Geologic/Geophysical, Historical - Well Constrained with Geological Background and Historical - Poorly Constrained with Geological Background categories, with the sole exception of the References.
The following scheme summarises the correspondence
between standard and virtual names for all of the Source Specific Support
Tables. "Corresponding file(s)" specifies the location of the tables
within the disk database.
| Table name/menu item | Corresponding file(s) | Content |
| Summaries of the Main Studies on the Source | Source_Literature
folder
Previous_Studies subfolder S-ITA-*.txt |
Summaries of papers (in chronological order) describing the source and its geologic and tectonic environment |
| Comments and Open Questions | Source_Literature
folder
Open_Questions subfolder Q-ITA-*.txt |
Summary of the compiler’s comments and of aspects of the source that still need to be investigated/understood |
| Pictures | Source_Literature
folder
Pictures subfolder F* sub-subfolder F*_*.tab F*_*_CAP.tab |
Published (scanned) or original pictures or photographs describing the source and its tectonic environment, and their caption containing a full reference to the source of the image |
| References | Source_Data
folder
Assign_References.tab |
References contained in the Database |
See also § 4.1.2. for a description of the
main characteristics of the Summaries of the Main Studies on the Source
and Comments and Open Questions
text files, § 4.1.3. for
a description of how to select
Pictures, § 2.2.4.4. and 4.1.4.
for guidelines concerning the
References.
2.2.5.2. Source Generic support tables
These tables contain information that relates indirectly to all the sources and that may be used to place them in their seismological, geologic and tectonic context.
The following scheme summarises the correspondence
between standard and virtual names for all of the Source Generic Support
Tables. By definition all these tables are also layers of the Geographic
Information System. "Colour" specifies the colour used to represent the
given graphic objects in the Geographic Information System; for scanned
images this field is omitted. "Corresponding file(s)" specifies the location
of the tables within the disk database; since all the support tables are
located in the folder Background_Info,
this information is omitted.
| Table name/menu item | Corresponding disk file(s) |
|
|
| Instrumental Earthquakes | Seismicity/Inst_q.tab |
|
|
Historical
Earthquakes:
|
Seismicity/CFTI_q.tab
Seismicity/CPTI_q.tab
Seismicity/NT_q.tab |
Vector
Vector
Vector |
Blue
Red
Violet |
Felt
Reports:
|
Seismicity/CFTIFelt.tab
Seismicity/NTFelt.tab
Seismicity/NTFelt.tab |
Vector
Vector
Vector |
Black/Red
Black/Red
Black/Red |
| Previous Fault Compilations | Geological/Compilations/
Compilations.tab
Geological/Compilations/Maps/ *.tab |
|
|
| Additional Geophysical/Seismological Data | Geological/
Additional_Data/Additional_Data_list.tab
Geological/Additional_Data/*.tab |
|
|
2.2.5.2.1. Seismological data: instrumental seismicity
Instrumental seismicity is taken from the monthly
bulletin of the Istituto Nazionale di Geofisica e Vulcanologia for the
period January 1985-December 2000. The information supplied by the Database
is a subset of the data that appear in the bulletin and retains the essential
parameters such as hypocentral coordinates, origin time, magnitude and
reliability of the solution. In particular, the Q1 and Q2
quality ratings range from A (most reliable) to D (least reliable) and
are assigned based on the epicentral uncertainties and on the network configuration
(azimuthal gap), respectively. Each earthquake is plotted as a solid white
circle. The diameter of the circle (in km) corresponds to the expected
source length obtained from the earthquake magnitude using Wells and
Coppersmith’s [1994] empirical relations.
2.2.5.2.2. Seismological data: historical seismicity
Historical seismicity is taken from the three largest compilations that were available at the end of 2000:
2.2.5.2.3. Previous Fault Compilations
The Previous Fault Compilations are figures from articles or from the web or printed maps containing active faults, seismogenic faults and lineaments. The figures are representative of a wide selection of investigators and areas and the only requisite for their inclusion in the Database was the correctness of the figure’s (map’s) geographic layout. Each figure/map was georeferenced with the maximum accuracy allowed by its quality. The results are generally satisfactory with a mismatch between the raster image and the GIS grid that usually does not exceed 3 km (5-10 km at the far edges of some larger scale compilations).
A full list of the Previous Fault Compilations that are presented with the first version of the Database is supplied in Appendix III.
Table structure: Compilations.tab
| Field name | Content | Format |
| Title | Title or short description of given compilation | Char(254) |
| Authors | Author(s) of given compilation (see table for adopted format) | Char(254) |
| Year | Year of publication of the given compilation | Char(16) |
| Reference | Full reference of journal, proceedings, volume or book were the given compilation was published. Journal titles should be abbreviated according to the World List of Abbreviations followed by volume number, first and last page (see table for adopted format) | Char(128)
|
| TableName | Name of table containing the given compilation | Char(128) |
| Compilation_ID | Encodes the given compilation by a progressive identification number | Char(16) |
2.2.5.2.4. Additional Geophysical/Seismological Data
The Database may be complemented by other geophysical and seismological data that are pertinent to the general problem of identifying seismogenic sources, characterising their behaviour, or simply placing them in their tectonic context for further elaboration or representation purposes. These layers of data are fully georeferenced and may be accompanied by substantial alphanumeric information associated with the graphic objects. This information can be accessed using MapInfo® standard tools (Info Tool) and bears no logic link with the rest of the textual information presented in the Database. The actual availability of this type of support information may vary depending on the specific release of the Database.
A full list of the Additional Geophysical/Seismological Data tables that are presented with the first version of the Database is supplied in Appendix IV.
Table structure: Additional_Data.tab
| Field name | Content | Format |
| Title | Title or short description of given set of additional data | Char(254) |
| Authors | Author(s) of given set of additioata (see table for adopted format) | Char(254) |
| Year | Year of publication (or preparation, if unpublished) of the given set of additional data | Char(16) |
| Reference | Full reference of journal, proceedings volume or book were the given set of additional data was published. Journal titles should be abbreviated according to the World List of Abbreviations followed by volume number, first and last page (see table for adopted format) | Char(128)
|
| TableName | Name of table containing the given set of additional data | Char(128) |
| ID | Encodes the given set of additional data by a progressive identification number | Char(16) |
2.2.5.3. Generic support tables
These tables contain information that may be used
to place all the seismological and tectonic information in their geographic
and administrative context. By definition, all these tables are also layers
of the Geographic Information System. In the following schemes "Colour"
specifies the colour used to represent the given graphic objects in the
Geographic Information System, "Corresponding file(s)" specifies the location
of the tables within the disk database. Since all the support tables are
located in the folder Background_Info,
this information is omitted.
2.2.5.3.1. Geographic and elevation data
The geographic interface of the
Database
is essentially based on a Digital Elevation Model of Italy with a regular
grid of about 240 m. This was re-sampled from a public-domain archive originally
compiled by Carrozzo et al. [1981]. The Digital Elevation Model
was re-processed to obtain a Colour Shaded Relief, a B/W Shaded
Relief and a
Colour Coded version. These can be used interchangeably
to emphasise specific features or to create the optimal contrast with the
rest of the information displayed. The Digital Elevation Model can also
be interchanged with a purely vectorial outline of Italy and surrounding
countries that leaves all its inland portions devoid of any topographic
information. The outline of European (except Italy) and North African countries
is displayed also in conjunction with any of the realisations of the Digital
Elevation Model.
The geographic interface is complemented by a
series of tables that outline with different shades of blue the bathymetry
of the seas surrounding Italy at 200, 500, 1,000, 2,000, 3,000 and 4,000
m depth. The bathymetry is automatically displayed in conjunction with
any of the realisations of the Digital Elevation Model (with shades of
grey for the B/W version).
The geographic grid is shown at fixed angular
intervals that change with the scale of representation from 0.1û
to 2û.
The drainage dataset is provided courtesy of
E.N.E.L./Hydro (former I.S.M.E.S.) and is represented at three different
levels of detail. The coarser level shows only the most important rivers
countrywide (normally, all those having a length in excess of 20 km). The
finest level includes most of the rivers and seasonal streams that can
be derived from a 1:25,000 scale map. The intermediate level contains a
selection of the latter and in particular all first and second order streams.
The following scheme summarises the correspondence
between standard and virtual names and the type of representation for all
of the geographic and elevation data.
| Table name/menu item | Corresponding disk file(s) |
|
|
Digital
Topography:
|
DEM/ShadedRelief/Ita*.tab
DEM/Bathymetry/*CC.tab Geographic/EuroMed.tab
DEM/ColourCoded/Ita*.tab DEM/Bathymetry/*CC.tab Geographic/EuroMed.tab
DEM/BW/Ita*.tab DEM/Bathymetry/*BW.tab Geographic/EuroMed.tab |
Vector Vector
Raster Vector Vector
Raster Vector Vector |
Palette Black
Palette Palette Black
Palette Palette Black |
Digital
Topography:
|
Geographic/EuroMed_Outline.tab |
Vector |
Black |
| Geographic Grid | Grids/Grid_*.tab |
|
|
Drainage:
|
Geographic/MainRiv.tab,Lakes.tab Geographic/InterRiv.tab,Lakes.tab Geographic/Idr*.tab,Lakes.tab |
Vector Vector Vector |
Blue Blue Blue |
2.2.5.3.2. Administrative data
Most of these data are provided by I.S.T.A.T. (Italian national agency in charge of countrywide statistics on economic and demographic data) and reflect the results of the 1991 national census. The layers Large Cities and Intermediate Cities include "capoluoghi di regione" and "capoluoghi di provincia", respectively. The SmallTowns layer includes 8,100 "comuni", the smallest territorial unit in the Italian public administration. The All Localities layer is supplied courtesy of E.N.E.L./Hydro (former I.S.M.E.S.) and includes 61,595 "frazioni", small settlements that are under the jurisdiction of a "comune". To learn what "comune" corresponds to a given "frazione" use the codes provided with the table or simply plot the "frazione" along with the layer Comuni_Borders.tab.
The following scheme summarises the correspondence
between standard and virtual names and the type of representation for all
of the administrative data.
| Table name/menu item | Corresponding disk file(s) |
|
|
| Administrative
Boundaries:
- Provinces - "Comuni" |
Administrative/Region_Borders.tab
Administrative/Province_Borders.tab Administrative/Comuni_Borders.tab |
Vector Vector Vector |
Black Black Black |
| Cities:
- Intermediate Cities - Small Towns ("Comuni") - All Localities ("Frazioni") |
Administrative/Large_Cities.tab
Administrative/Intermediate_Cities.tab Administrative/Small_Cities.tab Administrative/Small_Localities.tab |
Vector Vector Vector Vector |
Violet Orange Yellow Blue |
2.2.5.4. Summary of support tables
The following scheme summarises the different
categories of Support Tables, along with the indication of where
each specific layer of information is described in better detail.
| Category | Table name/menu item |
|
| Source Specific | Summaries of the Main Studies on the Source |
|
| Source Specific | Comments and Open Questions |
|
| Source Specific | Pictures |
|
| Source Specific | References |
|
| Source Generic | Instrumental Earthquakes |
|
| Source Generic | Historical
Earthquakes:
- from CFTI 3 catalogue - from CPTI catalogue - from NT4.1.1 Catalogue |
|
| Source Generic | Felt
Reports:
- from CFTI 3 catalogue - from NT 4.1.1/DOM (before 1900 AD) catalogue - from NT 4.1.1/DOM (since 1900 AD) catalogue |
|
| Source Generic | Previous Fault Compilations |
|
| Source Generic | Additional Geophysical/Seismological Data |
|
| Generic | Digital
Topography:
- Colour Shaded Relief - Colour Coded - B/W Shaded Relief - Outline Only |
|
| Generic | Geographic Grid |
|
| Generic | Drainage:
- Main Rivers Only - Main and intermediate - Full Drainage |
|
| Generic | Administrative
Boundaries:
- Regions - Provinces - "Comuni" |
|
| Generic | Cities:
- Large Cities - Intermediate Cities - Small Towns ("Comuni") - All Localities ("Frazioni") |
|