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Mr.Santosh Kumar Scientist Email: [email protected] Web: http:\\ www.isr.gujarat.gov.in

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  • Mr.Santosh Kumar Scientist

    Email: [email protected]

    Web: http:\\www.isr.gujarat.gov.in

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  • (ISR Established in 2006; New campus started 2008 end)

  • Seismology

    Active Tectonics

    Crustal

    Deformation

    Geophysics

    Earthquake Monitoring

    Source Mechanism

    Source Modeling

    Earthquake Geology

    Paleoseismology

    Recurrence Models

    GPS

    Tectonic Geomorphology

    Tsunami

    Gravity

    Magnetics

    Seismics

    GPR

    Strong motion

    Site-specific studies

    Microzonation

    Earthquake Engg.

    Ground Motion

    Three Main Groups

    Phys. of Earthquake process and Earths Structure

    Seismic Microzonation

    Earthquake Prediction Research

    DIRECTOR GENERAL

    INSTITUTE OF SEISMOLOGICSL RESEARCH

    Science and Technology Department

    Government of Gujarat

    Research Activitiess

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  • Seismograph, GPS and Land Survey INSTRUMENTS AT ISR

    Seismological Instruments:

    Broadband Seismographs (50) Strong Motion Accelerographs (50)

    Global Positioning Systems:

    Geodetic grade GPS (40)

    Land Survey Instruments:

    Real Time Kinematic GPS (2) Handheld GPS (2) Total Station (1)
  • Earthquake Recording Stations in Gujarat (by ISR)

    Central Recording Station at

    ISR-Gandhinagar

  • Seismic zoning Maps

    India

    Gujarat

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  • THE GUJARAT (INDIA) SEISMIC NETWORK (GSNet)

    50 Broadband seismographs (20 connected to ISR via VSAT), 50 Strong Motion Accelerographs

    50 Broadband seismographs and 50 strong motion accelerographs for precise locations and mechanism of earthquakes

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    50 Broadband seismographs and 50 strongmotion accelerographs for precise locations and mechanism of earthquakes

  • SEISMIC MONITORING

    50 Seismic Stations (nearly same as in the whole country) spread all over Gujarat.Av. 2.5 per district.20 connected by VSAT with at ISR, Gandhinagar .Epicenter & magnitude of earthquakes determined within 10 minutes of arrival of seismic waves round the clock.

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  • Instrumentation in GSNet

    The VSAT-connected seismograph stations have Gralp CMG 3T 120-s triaxial broadband sensors and Gralp CMG-DM24 24-bit digitizers with external GPSThe continuous data is recorded at 50 sps The strong-motion accelerographs consist of internal AC-63 GeoSIG triaxial forced balance accelerometers and GSR-18 GeoSIG 18-bit digitizers with external GPSThe recording is in trigger mode at 200 sps with threshold set at 0.002 g.The offline broadband seismograph stations are equipped with Gralp 120-s triaxial CMG-3T broadband sensors and Reftek 24-bit 130-01 digitizers with external GPS.Data are recorded in continuous mode at 100 sps.

    For more Information

    The Gujarat (India) seismic network (2008), Seismological Research Letters, 79 (6), 806-815

  • Noise Level

    The seismic stations of the network are located on varied geological formations including sandstone, basalt, shale, limestone, and hard soil of Mesozoic to Quaternary age

  • Data Processing

    Presently, all data processing is carried out in offline mode on SEISAN software (Havskov and Ottemller 2000). The online data are viewed on a 42-inch LCD monitor using the SCREAM (seismometer configuration, real-time acquisition and monitoring) application of GralpThe earthquakes are located with HYPOCENTRE utility and ML/mb/MS are calculated on the basis of distances.The components of individual stations are rotated, and spectral analysis is carried out for estimation of Mw and source parameters like seismic moment, fault radius, corner frequency, and stress drop

    Detection Capability

    The network recorded and located about 4,000 local earthquakes from July 2006 to OCT 2009 with magnitudes in the range of 0.5 to 5.0Local earthquakes are located with an error of 1-2 km in latitude and longitude and 45 km in depth.M2 is the detection capability in most parts of Kachchh, M3 in the mainland Gujarat and earthquakes of M 3 are well-recorded up to 200-km distance.The network can record earthquakes of M 4 within about 1,000 km, M 5 within about 2,000 km, M 5.5 within about 5,000 km, and M 6 within about 10,000 kmThe teleseismic earthquakes in the 2,0005,000-km range are located with an error of about 1 degree in latitude
  • A sample broadband record of an Mw 4.7 earthquake in the Kachchh region of Gujarat recorded at the Khavda (KAV0) station (epicentral distance 88 km) on 13 May 2007

  • A sample broadband record of an Ms 8.3 earthquake on 12 September 2007 in southern Sumatra, Indonesia, and recorded at the Kadana (KAD0) station (epicentral distance 5,024 km).

  • Location of earthquakes in Gujarat from historic times to 2009.

  • Earthquake epicenters located by GSNet during 2008

  • Location of earthquakes recorded by GSNet during the period July 2006 to June 2009

  • Long-term migration of seismicity in Kachchh, Gujarat

  • Map showing GPS station network of ISR for crustal deformation studies

    35 Permanent (red triangle- installed, green triangle- being installed)

    11 Campaign mode stations (blue dots)

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    20 permanent and several campaign mode GPS stations

  • Multi Parameter Geophysical Observatory ( MPGO) 3 Nos.

    Strain Meter 1 no.

    Supercondutivity Meter 1 no.

    Magnetometer 3no

    Water Level Measurement instrument 5 no

    Radon Gas Measurement 5 nos

    GPS

    BBS

    SMA

  • QUESTIONS?