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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.

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The Northern Cordilleran Mid-Cretaceous Plutonic Province: Ilmenite/Magnetite-series Granitoids and Intrusion-related Mineralisation

TL;DR: In this paper, magnetite-series plutonic suites and belts are defined across Alaska and Yukon, in the northern North American Cordillera, on the basis of lithological, geochemical, isotopic, and geochronometric similarities.
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Origin of lode-gold deposits of the Juneau gold belt, southeastern Alaska

TL;DR: In this article, the authors show that mesothermal gold-bearing quartz veins along the Juneau gold belt formed in the early Tertiary from H 2 O-CO 2 (±N 2,H 2 S,CH 4 )-rich, low-salinity fluids at temperatures of 200 to 325 °C and pressures in excess of 1 - 1.5 kbar.
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The giant Zaozigou Au-Sb deposit in West Qinling, China: magmatic- or metamorphic-hydrothermal origin?

TL;DR: In this article, two populations of monazite are identified within a mineralized dacite located along a major shear zone, and the Zaozigou Au-Sb deposit is best classified as an epizonal orogenic gold deposit.
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The conjunction of factors that lead to formation of giant gold provinces and deposits in non-arc settings

TL;DR: A hierarchical approach is required to progressively examine controlling parameters at successively decreasing scales in the total mineral system to understand the location of giant gold deposits in non-arc environments as mentioned in this paper.
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Secular Variation in Economic Geology

TL;DR: In this article, the authors focus on the temporal pattern of ore deposits on a constantly evolving Earth and the complex interplay between the evolving global tectonic regime, episodic mantle plume events, overall changes in global heat flow, atmospheric and oceanic redox states, and even singular impact and glaciation events.