2016-2017 USAP Field Season
Petrologic constraints on subduction termination from lamprophyres, Ross Orogen, Antarctica
Dr. John Cottle
University of California Santa Barbara
Project Web Site:
Supporting Stations: McMurdo Station
Rocks highly enriched in potassium such as lamprophyres potentially provide direct insight into foundering and the processes that occur during, and immediately after, termination of subduction. These enigmatic rocks are important because they represent near-primary mantle-melt compositions and therefore their age, geochemistry, and petrologic evolution reveal key information on both the composition of the upper mantle and its thermal state. Of equal importance, they reveal how these key parameters vary through both space and time. This project will study a suite of lamprophyres spanning approximately 1,300 kilometers along-strike and emplaced during the latest stages of the Neoproterozoic-Ordovician Ross Orogeny. High-precision geochronology, coupled with whole rock and mineral-scale elemental, isotope geochemical, and petrologic analysis, will elucidate the mechanisms for, and the temporal and spatial scales over which, deep crustal foundering/delamination occurred and the processes responsible for the significant isotopic heterogeneities observed in these rocks.
Field Season Overview
Field team members will travel by Basler aircraft to the Transantarctic Mountains where they will establish a light weight field camp in the Miller Range. After three weeks, they will make a camp move by Twin Otter aircraft to the Gabbro Hills through Shackleton Camp, at which time an ASC Field Safety Coordinator will join the team and the PI will depart. At both locations they will travel by foot and by snowmobile to collect rock samples and conduct geologic mapping. They will return to McMurdo via the Shackleton Field Camp. Samples will be returned to the home institution for analyses.
Deploying Team Members