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Ian Dalziel

Ian is one of two associate directors of UTIG and Professor of Geological Sciences at The University of Texas at Austin. He is a John J. and Katherine J. Jackson Research Fellow for 2002-2005. Ian has dedicated most of his career to understanding global tectonic processes and to mapping out the geography of ancient times on a dynamic Earth. His 35 years of field experience have been devoted to work in the British Caledonides, the Canadian Shield, the Andes, and Antarctica. NSF-sponsored fieldwork in Antarctica between 1995 and 1998 led Ian to propose that ancestral North America, known to

geologists as Laurentia, was connected to South America, Africa, and Antarctica one billion years ago by a large promontory, which he named the Texas Plateau. The results of this work were published in the January 1995 issue of Scientific American. Recently, working with colleagues from the U.K. and Australia, Ian has turned his attention to unraveling the complicated tectonic history of Scotland, his homeland. Ian was president of the International Division of Geological Society of America from 1996 to 1997, has served as delegate to the Scientific Committee on Antarctic Research of International Union of Geological Sciences since 1987, and has served as the International Secretary of the American Geophysical Union since 1996. [Dalziel web page]

 

Ron Steel

Ron's research aims at evaluating the signatures of tectonics, sea-level change and climate in fluvial, shallow marine and deepwater strata and has an important outcrop component. Current activity focuses on fluvial successions, shelf-margin deltas, tidal signatures and sandbodies, the process of transgression, improving the lowstand model, and fluvio-lacustrine systems. Ron is an AAPG Distinguished Lecturer for 2005. [Steel web page]

 

Sharon Mosher

Sharon's research involves structural petrology and field-oriented structural geology.  Her primary research interests are in the evolution of complexly deformed terranes, strain analysis, deformation mechanisms, and the interaction between chemical and physical processes during deformation. Sharon currently has four active research areas: the Mesoproterozoic of Texas, the Australian-Pacific oceanic plate boundary south of New Zealand, northwest Highlands of Scotland, and the southwestern U.S. Mesozoic Maria Tectonic belt. Sharon is a past President of GSA. [Mosher web page]

 

Randall Marrett

Randy's research concentrates on deformation processes in the upper continental crust where folds, faults, and opening-mode fractures are the most important products. This work is applicable to a wide range of human concerns such as natural hazards (e.g., earthquakes, volcanoes) and the flow of fluids through rock (e.g., hydrocarbons, water, contaminants). Some common themes that relate his disparate interests are quantitative field observations and analysis, especially using techniques that address spatial and size scaling of structures.

Randy currently has on-going projects that address active faulting and geyser eruption patterns in the Central Andes of Argentina and Chile, detachment folding and curved orogenic belt development in the Sierra Madre Oriental of Mexico, and opening-mode fracturing in numerous areas. Randy is an Associate Professor in the Department of Geological Sciences. [Marrett web page]

 

Don Blankenship

Don uses both airborne and ground-based geophysical techniques, including laser altimetry, radar sounding, seismic reflection and refraction, and potential fields methods, to investigate dynamics of large ice sheets and subglacial geology. Much of his current research is focused on understanding the West Antarctic rift system (including the flanking Transantarctic Mountains) and the marine-based West Antarctic Ice Sheet. Blankenship's recent aerogeophysical investigations have verified that there is a strong correlation between

subglacial sediments and ice streaming; these airborne experiments also give indications of active subglacial volcanism near the critical region where ice streams begin. The airborne platform that he developed to simultaneously acquire ice-penetrating radar, laser altimetry, airborne gravity, and aeromagnetic measurements has become the foundation for an NSF-sponsored national facility for airborne geophysics in Antarctica (SOAR) operating from UTIG. Building on his expertise in radar sounding and ice sheets, Blankenship is involved in the planning of an unmanned space mission to Europa, one of Jupiter's moons, which is thought to have an ice-covered ocean that may host exotic life. He has served on several definition teams for NASA's Europa Orbiter Mission, currently planned to launch in 2006. Don is a Research Scientist at the Insitute for Geophysics. [Blankenship web page]

 

Steve Laubach

Steve uses quantitative petrographic and other microstructural observations and principles of structural geology and diagenesis to address questions about chemical and mechanical interactions in sedimentary basins and processes of fracturing and rock deformation. Fractures and associated diagenetic features play important roles governing the success of attempts to access natural resources in deeply buried sedimentary rocks. Yet because fractures are challenging to sample and have deceptively simple morphology,

they remain among the least well-understood geologic structures. Steve is currently engaged in research in the western United States, northeastern Mexico, Colombia, Argentina, Texas, and northwest Scotland. Steve is a Senior Research Scientist in the Bureau of Economic Geology and a John J. and Katherine J. Jackson Research Fellow for 2003-2005. He was an SPE Distinguished Lecturer in 2004. Steve is the Principal Investigator for the JSG Scotland Field Workshop project. [Laubach web page]

 

 

JSG Scotland 2005 is funded by the Geology Foundation of the John A. and Katherine G. Jackson School of Geosciences.