Fraser Goff

University of New Mexico, Albuquerque, NM, United States 
"Fraser Goff"
Mean distance: 19906.5
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Cisneros-Dozal LM, Huang Y, Heikoop JM, et al. (2014) Assessing the strength of the monsoon during the late Pleistocene in southwestern United States Quaternary Science Reviews. 103: 81-90
Goff F, Warren RG, Goff CJ, et al. (2014) Eruption of reverse-zoned upper Tshirege Member, Bandelier Tuff from centralized vents within Valles caldera, New Mexico Journal of Volcanology and Geothermal Research. 276: 82-104
Kelley SA, McIntosh WC, Goff F, et al. (2013) Spatial and temporal trends in pre-caldera Jemez Mountains volcanic and fault activity Geosphere. 9: 614-646
Wilcock J, Goff F, Minarik WG, et al. (2013) Magmatic recharge during the formation and resurgence of thevalles caldera, new mexico, usa: Evidence from quartz compositional zoning and geothermometry Journal of Petrology. 54: 635-664
Marques JM, Carreira PM, Goff F, et al. (2012) Input of 87Sr/ 86Sr ratios and Sr geochemical signatures to update knowledge on thermal and mineral waters flow paths in fractured rocks (N-Portugal) Applied Geochemistry. 27: 1471-1481
Fawcett PJ, Werne JP, Anderson RS, et al. (2011) Extended megadroughts in the southwestern United States during Pleistocene interglacials. Nature. 470: 518-21
Albrecht M, Goff F, Gardner JN, et al. (2011) Multi-disciplinary and integrated geothermal exploration at the Pueblo of Jemez, New Mexico Transactions - Geothermal Resources Council. 35: 677-682
Marques JM, Matias MJ, Basto MJ, et al. (2010) Hydrothermal alteration of Hercynian granites, its significance to the evolution of geothermal systems in granitic rocks Geothermics. 39: 152-160
Gardner JN, Goff F, Kelley S, et al. (2010) Rhyolites and associated deposits of the Valles-Toledo caldera complex New Mexico Geology. 32: 3-18
Chipera SJ, Goff F, Goff CJ, et al. (2008) Zeolitization of intracaldera sediments and rhyolitic rocks in the 1.25 Ma lake of Valles caldera, New Mexico, USA Journal of Volcanology and Geothermal Research. 178: 317-330
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