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OBS Program at UTIG

UTIG
Ocean-Bottom Seismometer Program

A UTIG OBS
being deployed

A UTIG OBS
being recovered

Post-recovery
cleanup


UTIG investigators apply seismic refraction surveying to a wide range of problems, from large-scale experiments designed to study the structure of the entire crust, to investigations of targeted geologic settings. Seismic refraction surveying utilizes seismic energy that returns to the surface after traveling through the ground along refracted ray paths. The refracting interfaces (refractors) separate layers of different seismic velocity. Sound travels at different speeds through different types of rocks and seismologists can use these data to develop detailed images of the crust and the upper mantle below the seafloor.

To carry out seismic refraction work on the seafloor, UTIG has developed a specialized ocean-bottom seismometer (OBS). This is a microprocessor- controlled instrument that is placed on the seafloor to record seismic signals generated by seismic sources. The OBS instrument and control electronics are contained in a glass ball (sphere) encased in a yellow polyethylene housing called a hard hat. The instrument is deployed from a surface ship, free-falls to the seafloor, and while on the seafloor detects and records seismic signals. Commercially available hard disks store the data in the instrument. Experiments may be passive, in which the energy generated by earthquakes is detected and used to create an image of the Earth's interior, or active, in which a sesimic source (i.e. sound) is generated from research ships. After the data acquisition is completed, the system receives a sound signal from a surface ship, which triggers the OBS to release itself from the seafloor and float to the surface for recovery.  On board the ship, the data can be downloaded to standard computer workstations and evaluated. UTIG researchers are currently using OBS instruments in offshore seismic investigations with diverse geological/geophysical targets in many parts of the world.

A sample record section from offshore Costa Rica illustrates OBS data collection.

In 1999, a lost OBS was found - 20 months and across the Atlantic Ocean from where it was last seen.

Since 1995, UTIG has made 394 OBS deployments at 9 experiment sites. Listed below are some of the recent studies using the instruments.

Project

Principal Investigators

Year

#Deployments

SE Caribbean Margin

Christeson, Mann

2004

 

Shear Wave Studies of Hydrate Ridge

Bangs, Pecher

2002

 

Bransfield Strait

Austin, Christeson, Dalziel, Nakamura

2000

99

Hydrate Ridge, Oregon Continental Margin

Bangs, Sen, Nakamura

2000

 

Nicaragua Subduction Factory

McIntosh

2000

 

Hydrate Ridge Project

Bangs, Nakamura

2000

21

A New Generation of
Broadband Ocean Bottom Seismograph

Pulliam, Nakamura

1999

1

Lesser Antilles Subduction Zone

Bangs

1998

32

Iberia Continental Margin

Austin, Nakamura

1997

33

Chicxulub KT Impact Crater, Yucatan

Buffler

1996

34

Northwest shelf of Australia

Nakamura

1995-96

91

Taiwan Arc Continent Collision

McIntosh, Nakamura

1995

39

Upper Plate Response to Subducting Plate

Mcintosh

1995

44


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