J
Jeffrey Lee
Researcher at Central Washington University
Publications - 58
Citations - 2901
Jeffrey Lee is an academic researcher from Central Washington University. The author has contributed to research in topics: Shear zone & Metamorphism. The author has an hindex of 32, co-authored 51 publications receiving 2607 citations. Previous affiliations of Jeffrey Lee include Monash University, Clayton campus & California Institute of Technology.
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Evolution of the Kangmar Dome, southern Tibet: Structural, petrologic, and thermochronologic constraints
Jeffrey Lee,Bradley R. Hacker,William S. Dinklage,Yu Wang,Phillip B. Gans,Andrew J. Calvert,JingLin Wan,Wenji Chen,Ann E. Blythe,William C. McClelland +9 more
TL;DR: In this paper, structural, thermobarometric, and thermochronologic investigations of the Kangmar Dome, southern Tibet, suggest that both extensional and contractional deformational histories are preserved within the dome.
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Constraints on present‐day Basin and Range deformation from space geodesy
TL;DR: In this article, the authors used space geodetic data from very long baseline interferometry and satellite laser ranging combined with other geodesic and geologic data to study contemporary deformation in the Basin and Range province of the western United States.
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Onset of mid-crustal extensional flow in southern Tibet: Evidence from U/Pb zircon ages
Jeffrey Lee,Martin J. Whitehouse +1 more
TL;DR: In this article, an ion microprobe U/Pb dates from zircon in deformed orthogneiss and migmatite and an undeformed granite in Mabja Dome are the first to constrain the timing of peak metamorphism, and onset and duration of mid-crustal ductile extension, in southern Tibet at 35.0 ± 0.8 Ma and ∼12-19 million years.
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Evolution of North Himalayan gneiss domes: structural and metamorphic studies in Mabja Dome, southern Tibet
TL;DR: In this article, structural and metamorphic petrology investigations of Mabja gneiss dome, southern Tibet, suggest that contractional, extensional, and diapiric processes contributed to the structural evolution and formation of the domal geometry.
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Do microplates in subduction zones leave a geological record
Joann M. Stock,Jeffrey Lee +1 more
TL;DR: In this article, the authors apply these observations to boundaries of the Arguello, Monterey, Guadalupe, and Magdalena microplates, which existed in the subduction zone west of Baja California at various times from 20 to 12.5 Ma.