1. Mesozoic tectonics and metamorphism in the Wood Hills and Pequop Mountains region, northeast Nevada: implications for the architecture and evolution of the Sevier orogen;Camilleri;Geological Society of America Bulletin,1997
2. Camilleri, P. A. (1994) Mesozoic and Cenozoic tectonic and metamorphic evolution of the Wood Hills and Pequop Mountains, Elko County, Nevada. Unpublished Ph.D. thesis. University of Wyoming
3. Camilleri, P. A., Miller, D. M., Snoke, A. W. and Wells, M. E. (1992) Structure and fabric of metamorphic terrains in the northeastern Great Basin: Implications for Mesozoic crustal shortening and extension. In Field guide to geologic excursions in Utah and adjacent areas of Nevada, Idaho, and Wyoming, ed. J. R. Wilson, pp. 19–58. Utah Geological Survey Miscellaneous Publication, 92
4. Pressure–temperature–time paths of regional metamorphism I. Heat transfer during the evolution of regions of thickened continental crust;England;Journal of Petrology,1984
5. Thermal evolution of a portion of the Sevier hinterland: the northern Ruby Mountains–East Humboldt Range and Wood Hills, northeastern Nevada;Hodges;Tectonics,1992