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Structural Geology and Tectonics draws on all geoscience disciplines to address fundamental questions about plate tectonic and deformation processes. In recent years, there has been an explosion of new technologies which allow scientists to answer questions that were once beyond their reach. This research not only leads to advances in basic research, but is also relevant to society, through the exploration for natural resources and understanding of natural hazards.

Structural Geology and Tectonics research at the Jackson School spans the entire spectrum from continental to oceanic and upper crustal to mantle tectonics. Only a handful of programs in the country cover such a wide range. Researchers investigate processes at all scales using field and marine geophysical-based observations; laboratory-based petrologic, geochronological, structural and geochemical analyses; and theoretical and physical modeling.

Tectonically-focused research addresses processes at active and ancient plate boundaries. At convergent margins, research topics range from subduction zone processes to interactions among volcanic arcs, subduction zones and continents, including collision, uplift, and basin evolution. Extensional tectonic processes under investigation range from continental extension in the deep to shallow crust to evolution of passive margins, spreading ridges, and oceanic crust. Other research concentrates on the evolution of transitional plate boundaries as well as transform boundaries. The Jackson School also has a large research program investigating Precambrian tectonics and plate reconstructions, including using such orogens to study evolution of the deep crust.

Other major research areas focus on deformation processes including thin-skinned fold and thrust belt processes and associated fluid flow; formation of salients; salt tectonics; and strain partitioning in extensional and contractional shear zones. Another major research focus is on understanding fracturing, fracture processes, fractured reservoirs and relationships to diagenesis and fluid flow.

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  • California: evolution of the Franciscan subduction complex, Great Valley forearc basin, and the transition to transform tectonics.
  • Southwestern US: structural and metamorphic evolution of the Mesozoic Maria fold and thrust belt; initiation of unroofing and formation of corrugations on metamorphic core complexes
  • Texas: investigation of Grenville age Llano and west Texas uplifts; petrologic, structural, and geochronologic studies of granitic, ultramafic, and metamorphic rocks in the collisional orogen core and transpression and focused fluid flow in the foreland
  • Sierra Madre, Mexico: structural research on detachment folding, opening-mode fractures and faults, and formation of salients in thin-skinned fold and thrust belt
  • Central Andes: coupling between active deformation and magmatism
  • Indonesia: tectonics and petrology of the Ertsberg (Gunung Bijih) copper-gold district, west New Guinea; seismic imaging and tectonic interpretation in the area of the great Sumatran earthquake
  • Southwestern Australia, Greenland, Scandinavia, Eastern Canada, North Africa: evolution of the deep crust along plate margins
  • Fracturing and fractured reservoirs: field and microscopic observation of fracture populations; analysis of fracture scaling and reservoir properties.
  • Strain partitioning in shear zones in contractional and extensional orogens
  • Macquarie Ridge Complex: transition of the Australia-Pacific plate boundary sout of New Zealand from a spreading ridge to a transform plate boundary and locally to an incipient subduction zone.
  • Japan: 3-D seismic imaging, interpretation, and integration with upcoming Nankai Trough Seismogenic Zone (NanTroSEIZE) drilling project of the Integrated Ocean Drilling Program (IODP)
  • Alaska: Reflection and refraction studies of the Yakuata microplate collision and the tectonic-climatic interactions of the St. Elias orogeny
  • Taiwan: Onshore-offshore seismic study of the Taiwan orogen
  • Active tectonics and seismic hazards in the circum-Caribbean region: remote sensing, field-based fault mapping, shallow geophysical studies of coastal regions, tectonic geomorphology of subaerial and submarine faults, trenching of subaerial faults, tsunami-related studies.
  • Antarctica and southern South America: tectonics and GPS instrumentation of the southern continents and ocean.
  • Arctic Ocean: Investigations of the tectonic origin of the Arctic Ocean basin
  • Arctic Canada: interplay of salt tectonics and tectonostratigraphy in the Sverdrup Basin in the context of regional plate tectonics since the Carboniferous.
  • Gulf of Mexico: mechanisms and kinematics of Neogene thrust advance of the Sigsbee Escarpment along the abyssal deformation front of the Louann salt basin.
  • Eastern Mediterranean: Neogene interplay between extension and shortening in multilayered Messinian evaporites on the Levant continental margin.
  • Gulf of Mexico: three-dimensional kinematics of salt-canopy systems of the mid-slope region.
  • Seismic stratigraphy, structure, and hydrocarbon potential of the Caribbean and Gulf of Mexico basins using a combination of data collected by academic surveys and data collected by the oil industry.
  • Using sedimentary provenance studies to constrain tectonic reconstructions in the circum-Caribbean area.

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Few programs in the country have an array of analytical instruments as comprehensive as that in the Jackson School. All facilities and equipment are available for student research.

The equipment includes: a unique high-resolution X-ray CT scanner; an electron microprobe; two scanning electron microscopes with EDS, EBSD, and CL capabilities; a quadrupole ICPMS and a magnetic-sector ICPMS, both with laser-ablation capabilities; two mass spectrometers for stable isotopic studies; and a TIMS for radiogenic isotopic analyses. For field and geophysical research, the program operates: a new portable high-resolution seismic imaging system, portable seismographs, ground penetrating radar, LIDAR, a gravimeter, seismic sources, GPS receivers, portable magnetometers, an aero-geophysical instrument package and an ocean bottom seismometer system. There are also dedicated laboratories for stable and radiogenic isotopic analysis, paleomagnetic analysis, experimental petrology and physical modeling.

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Students in this program receive mentoring in all aspects of becoming a professional in Structural Geology and Tectonics, including conducting research; publishing in peer reviewed journals; presenting at national and international meetings; and teaching. Students leaving the program are well prepared for work in academia, research labs and industry.

“I was able to work with the best people in my field of interest ... In addition, my interactions with my mentors provided me with opportunities that I don't think could have been repeated very easily at other places. In my case, I was able to work in an area of the Andes mountains that very few people in the world get to visit, let alone investigate scientifically. The opportunities I received at Texas gave me experiences that are among the most valuable in my life.” – Keith Klepeis, Associate Professor, Dept. of Geology, University of Vermont

“The part of my graduate experience that most prepared me for my current work was the diversity in my experience. I'm doing projects now I never dreamed I'd have undertaken while there.” – Robert Roback, Team Leader, Radionuclide Geochemistry, Earth and Environmental Sciences Division, Los Alamos National Laboratory

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Researchers and students in this program area routinely work in the western U.S., Mexico, Antarctica, South America, Australia, Indonesia, Pacific rim, Caribbean, Greenland, Labrador, Scandinavia, and Scotland.

Research opportunities are greatly expanded due to two affiliated institutions: the Institute for Geophysics and the Bureau of Economic Geology, the latter of which functions as the state geological survey. These institutions house, for example, the following research groups: CBTH (Caribbean Basins, Tectonics & Hydrocarbons); PLATES (Plate Tectonics); the Fractures Group; and the Salt Tectonics Group.

Students in this area have the opportunity to do research in a broad range of field settings, including modern and ancient mountain belts around the world and aboard ocean-going research cruises to conduct marine geophysical investigations of active plate boundaries. Students also investigate tectonic and deformation processes in the laboratory using state of the art tools for geochronology, geothermobarometry, 3D imaging and physical modeling.

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