The presence of hot, weak crust is a central component of recent hypotheses that seek to explain the evolution of continent-continent collisions, and in...
Recognition and subsequent study of the syn-convergent low-angle normal faults and shear zones - the South Tibetan Detachment System (STDS) - that form the...
The Wager shear zone (WSZ) is a major east- or west-trending zone of high strain located on the northwestern coast of Hudson Bay. New geological mapping was...
We used in situ laser-ablation split-stream petrochronology to target monazite and xenotime associated with specific metamorphic index minerals in the Florence...
A newly identified and dated segment of the South Tibetan detachment in the Karnali klippe, western Nepal Himalaya, constrains initiation of mid-crustal...
Geologic mapping accompanied by microstructural and geochronologic analyses from the lower Himalayan metamorphic core in west-central Nepal record along-strike...
The Tibetan plateau is host to numerous ~N-S striking graben that have accommodated E-W directed extension. The development of these structures has been...
Structural analysis, petrochronology and metamorphic petrology enable identification and bracketing of the timing of a newly mapped high-temperature ductile...
The exposed mid-crustal rocks of the Himalayan orogen provide a natural laboratory for constructing the kinematic evolution of the midcrust during a...
Although the India-Asia collision has been ongoing since the Eocene, the exposed hinterland of the Himalayan orogen was pervasively deformed and metamorphosed...
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