27
Cuban Seismic Network National Centre for Seismological Research (2010) . Eduardo R. Diez Zaldívar. tro Nacional de Investigaciones Sismológicas. AIS. isterio de Ciencia, Tecnología y Medio Ambiente. MA. A.

Cuban Seismic Network National Centre for Seismological Research (2010) Ing. Eduardo R. Diez Zaldívar. Centro Nacional de Investigaciones Sismológicas

Embed Size (px)

Citation preview

Page 1: Cuban Seismic Network National Centre for Seismological Research (2010) Ing. Eduardo R. Diez Zaldívar. Centro Nacional de Investigaciones Sismológicas

Cuban Seismic Network

National Centre for Seismological Research (2010)

Ing. Eduardo R. Diez Zaldívar.Centro Nacional de Investigaciones Sismológicas.CENAIS.Ministerio de Ciencia, Tecnología y Medio Ambiente.CITMA.CUBA.

Page 2: Cuban Seismic Network National Centre for Seismological Research (2010) Ing. Eduardo R. Diez Zaldívar. Centro Nacional de Investigaciones Sismológicas

Cuba is part of the North American plate and lies on its boundary with the Caribbean one,

Page 3: Cuban Seismic Network National Centre for Seismological Research (2010) Ing. Eduardo R. Diez Zaldívar. Centro Nacional de Investigaciones Sismológicas

The beginning of the known seismic history of Cuba came with the Spanish settlements in the XVI century, and since that time several major and large earthquakes are reported in Greater Antilles.In the last five centuries, the eastern Cuban territory was affected by 26 earthquakes with intensity VI degrees or more, the most importance’s where 17 with VII degrees, 7 7 earthquakes with VIII earthquakes with VIII degrees and 2 with IX degrees and 2 with IX degrees.degrees.

Page 4: Cuban Seismic Network National Centre for Seismological Research (2010) Ing. Eduardo R. Diez Zaldívar. Centro Nacional de Investigaciones Sismológicas

During May and June, 2010, was installed new equipments acquired in the People Republic of China.

Mainly, was kept the idea of one national broad band network (7 stations), with 120 and 60 seconds BB seismometers, in order to record not only a local seismicity but also regional and tele-seismic earthquakes.

Also, a short period radio telemetric network was installed for more specific studies with local seismicity and in the stations close to main fault system, in addiction with seismometer, we connected some strong motion accelerometers.

Page 5: Cuban Seismic Network National Centre for Seismological Research (2010) Ing. Eduardo R. Diez Zaldívar. Centro Nacional de Investigaciones Sismológicas

The new networks are connected to the central station using ADSL modems, radio telemetry and some satellite links, depending of connectivity, topography, distances and INTERNET facilities.

Page 6: Cuban Seismic Network National Centre for Seismological Research (2010) Ing. Eduardo R. Diez Zaldívar. Centro Nacional de Investigaciones Sismológicas

With automatic phase pick-up software and on-line epicenter location with magnitude calculation, it is possible to offer fast results with information about the energetic-spatially earthquake parameters.Also, all stations will be, in the next future, full open for data interchange, in order to collaborate with scientific and research institutions from neighboring countries.

Short period radio telemetric network

Page 7: Cuban Seismic Network National Centre for Seismological Research (2010) Ing. Eduardo R. Diez Zaldívar. Centro Nacional de Investigaciones Sismológicas

1. Broad band stations.

Page 8: Cuban Seismic Network National Centre for Seismological Research (2010) Ing. Eduardo R. Diez Zaldívar. Centro Nacional de Investigaciones Sismológicas

BBVS60 and BBVS120 Seismometers (similar to REFTEK “Observer” model 151-120 and 151-60).

Page 9: Cuban Seismic Network National Centre for Seismological Research (2010) Ing. Eduardo R. Diez Zaldívar. Centro Nacional de Investigaciones Sismológicas

Dynamic range and frequency response of BBVS60 (top) and BBVS120 (botton).

Page 10: Cuban Seismic Network National Centre for Seismological Research (2010) Ing. Eduardo R. Diez Zaldívar. Centro Nacional de Investigaciones Sismológicas

Accelerometer BBAS-2 (Strong motion).

Page 11: Cuban Seismic Network National Centre for Seismological Research (2010) Ing. Eduardo R. Diez Zaldívar. Centro Nacional de Investigaciones Sismológicas

EDAS-24IP, 3 or 6 channel datalogger with 24 bits dynamic range, GPS time, TCP-IP protocol support, 8 Gbytes internal storage capacity and LINUX inside.

Page 12: Cuban Seismic Network National Centre for Seismological Research (2010) Ing. Eduardo R. Diez Zaldívar. Centro Nacional de Investigaciones Sismológicas

MGV, CCC and SOR Broad band stations

Page 13: Cuban Seismic Network National Centre for Seismological Research (2010) Ing. Eduardo R. Diez Zaldívar. Centro Nacional de Investigaciones Sismológicas

2. Short period network.

Page 14: Cuban Seismic Network National Centre for Seismological Research (2010) Ing. Eduardo R. Diez Zaldívar. Centro Nacional de Investigaciones Sismológicas

Short period seismometer FSS-3M Frequency and

phase response.

Page 15: Cuban Seismic Network National Centre for Seismological Research (2010) Ing. Eduardo R. Diez Zaldívar. Centro Nacional de Investigaciones Sismológicas

SAB, RCC and PIN Short period stations

Page 16: Cuban Seismic Network National Centre for Seismological Research (2010) Ing. Eduardo R. Diez Zaldívar. Centro Nacional de Investigaciones Sismológicas

Include WINDOWS server, SCO UNIX open server and database-interchange server.

Page 17: Cuban Seismic Network National Centre for Seismological Research (2010) Ing. Eduardo R. Diez Zaldívar. Centro Nacional de Investigaciones Sismológicas

General idea for server interactions.

Page 18: Cuban Seismic Network National Centre for Seismological Research (2010) Ing. Eduardo R. Diez Zaldívar. Centro Nacional de Investigaciones Sismológicas

Real-Time Data Processing System Interactive Data Analysis Software Strong Motion Data Analysis Software Data Exchange Server Real-Time Monitor System Seismic Data Manage System

Page 19: Cuban Seismic Network National Centre for Seismological Research (2010) Ing. Eduardo R. Diez Zaldívar. Centro Nacional de Investigaciones Sismológicas

Two main acquisition software, one in WINDOWS, another in SCO (duplicate).

Windows acquisition software.

SCO UNIX acquisition software.

Page 20: Cuban Seismic Network National Centre for Seismological Research (2010) Ing. Eduardo R. Diez Zaldívar. Centro Nacional de Investigaciones Sismológicas

Used for analysis the seismic data and locate the earthquake

Main Function: Read the data file recorded by the Real-Time Data Processing

System and display the wave data. Pick the phase. Locate earthquake and display the hypocenter on the map. Data process: Filter, Emulating data to Wood-Anderson

seismometer record. Convert the data file to SAC or SEED file format.

Operating System: SCO Open Server 6.0 Windows XP/2003 Server/VISTA

2. Interactive Data Analysis Software.

Page 21: Cuban Seismic Network National Centre for Seismological Research (2010) Ing. Eduardo R. Diez Zaldívar. Centro Nacional de Investigaciones Sismológicas

Interactive analysis software EDSP-IAS for earthquake analysis.

Page 22: Cuban Seismic Network National Centre for Seismological Research (2010) Ing. Eduardo R. Diez Zaldívar. Centro Nacional de Investigaciones Sismológicas

Epicenter location and earthquake parameter calculation using EDSP-IAS software.

Page 23: Cuban Seismic Network National Centre for Seismological Research (2010) Ing. Eduardo R. Diez Zaldívar. Centro Nacional de Investigaciones Sismológicas

Used for analysis the strong motion acceleration data.

Main Function: Read the strong motion acceleration data file recorded by the Real-time

Data Processing System. Data Process:

• Data correction.• Compute the velocity and the displacement data with the acceleration

data.• Compute the time duration and PGA.• Filter.• Compute the noise-signal spectrum.• Spectral processing for acceleration, velocity and displacement data.• Response spectrum for acceleration, velocity and displacement data.• Calculate intensity.

Print graph. Save as the wave data or spectrum to another file.

3. Strong Motion Data Analysis Software.

Page 24: Cuban Seismic Network National Centre for Seismological Research (2010) Ing. Eduardo R. Diez Zaldívar. Centro Nacional de Investigaciones Sismológicas

Acceleration record

Response Spectrum for acceleration

Page 25: Cuban Seismic Network National Centre for Seismological Research (2010) Ing. Eduardo R. Diez Zaldívar. Centro Nacional de Investigaciones Sismológicas

Main Function: Realize the data share between the subsystem or the seismic network

real-timely. The shared data includes:

• Real-time wave data.• Seismic information.• Digital seismic station running status.• Software running status.• Network communication status.

4. Data exchange Server.

Page 26: Cuban Seismic Network National Centre for Seismological Research (2010) Ing. Eduardo R. Diez Zaldívar. Centro Nacional de Investigaciones Sismológicas
Page 27: Cuban Seismic Network National Centre for Seismological Research (2010) Ing. Eduardo R. Diez Zaldívar. Centro Nacional de Investigaciones Sismológicas

THANK YOU!!!

[email protected]