2003-2004 USAP Field Season

Geology & Geophysics

Dr. Rama K. Kotra
Program Manager

G-079-M

NSF/OPP 02-30285
Station: McMurdo Station
RPSC POC: Curt LaBombard
Research Site(s): Transantarctic Mountains
Dates in Antarctica: Late October to early February

Transantarctic Mountains deformation network: GPS measurements of neotectonic motion in the antarctic interior
Dr. Terry J. Wilson
Ohio State University
Geological Sciences and Byrd Polar
twilson@mps.ohio-state.edu
http://www.geology.ohio-state.edu/TAMDEF
 
 
Photo not available.
Deploying Team Members: Graeme Blick . Robert Glover . Donald B. Grant . Dorota Grejner-Brzezinska . Larry D. Hothem . Sarah Morris . Michael J. Willis . Terry J. Wilson . Jan Wuite . Yi Yudan
Research Objectives: We will conduct global positioning system (GPS) measurements of bedrock crustal motions in an extension of the Transantarctic Mountains Deformation Network (TAMDEF) in order to document neotectonic displacements caused by tectonic deformation within the West Antarctic Rift or mass changes in the antarctic ice sheets. By monitoring the U.S. and Italian networks of bedrock GPS stations along the Transantarctic Mountains and on offshore islands in the Ross Sea, we will tightly constrain horizontal displacements related to active neotectonic rifting, strike-slip translations, and volcanism. We will use GPS-derived crustal motions, together with information from other programs on the ice sheets and from ongoing structural and seismic investigations in Victoria Land, to model glacio-isostatic adjustments due to deglaciation and to modern mass changes in the ice sheets. The integrative and iterative nature of this modeling will yield a holistic interpretation of neotectonics and ice sheet history that will help us discriminate tectonic crustal displacements from viscoelastic/elastic glacio-isostatic motions.

We will do repeat surveys of key sites southward about 250 kilometers along the Transantarctic Mountains. These measurements will cross gradients in predicted vertical motion due to viscoelastic rebound. The southward extension will also allow us to determine the southern limit of the active Terror Rift and will provide a better baseline for constraints on any ongoing tectonic displacements across the West Antarctic Rift system as a whole. Further, we will investigate unique aspects of GPS geodesy in Antarctica to determine how the error spectrum compares with that found in mid-latitude regions and to identify optimum measurement and data processing methods. The geodetic research will improve position accuracies within our network and will also yield general recommendations for other deformation-monitoring networks in polar regions.

An education and outreach program targeted at Ohio State University undergraduates who are not science majors will illuminate the research process for nonscientists. This effort will educate students about science and inform them about Antarctica and how it relates to global science issues.