R
Richard J. Goldfarb
Researcher at China University of Geosciences (Beijing)
Publications - 155
Citations - 13576
Richard J. Goldfarb is an academic researcher from China University of Geosciences (Beijing). The author has contributed to research in topics: Terrane & Craton. The author has an hindex of 48, co-authored 148 publications receiving 11462 citations. Previous affiliations of Richard J. Goldfarb include Denver Federal Center & University of Western Australia.
Papers
More filters
OtherDOI
Chemical analyses of ground and surface waters, Ester Dome, central Alaska, 2000-2001
Journal ArticleDOI
The Mustajarvi orogenic gold occurrence, Central Lapland Greenstone Belt, Finland: a telluride-dominant mineral system
TL;DR: Mustajarvi gold occurrence lies in the southern part of the Paleoproterozoic Central Lapland Greenstone Belt, in proximity to the first-order transcrustal Venejoki thrust fault system as mentioned in this paper.
Book ChapterDOI
Exploration for Komatiite-Associated Ni-Cu-(PGE) Mineralization in the Thompson Nickel Belt, Manitoba
D. Layton-Matthews,C. M. Lesher,O. M. Burnham,Larry J. Hulbert,David C. Peck,J. P. Golightly,Reid R. Keays,Richard J. Goldfarb,Erin E. Marsh,Monecke Thomas +9 more
Journal ArticleDOI
The role of exhumation in the temporal distribution of ore deposits—a discussion
TL;DR: Kesler and Wilkinson as discussed by the authors used a modal age of 160 ± 15 Ma for exposed orogenic gold deposits, which is a period in Earth history when there are few, if any, absolute dates for large orogeni gold deposits.
Journal ArticleDOI
Structural evolution of a gold-bearing transtensional zone within the Archean Porcupine-Destor deformation zone, southern Abitibi greenstone belt, eastern Ontario, Canada
Miguel Tavares Nassif,Yvette D. Kuiper,Richard J. Goldfarb,Thomas Monecke,Christopher S. Holm-Denoma +4 more
TL;DR: In situ U-Pb laser ablation-inductively coupled plasma-mass spectrometry performed on monazite grains formed within the shear fabric of the Munro deformation zone indicates that transtension occurred at 2657±µ15µMa.