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Re-Os age of the Pueblo Viejo epithermal deposit, Dominican Republic

Jason D. Kirk, Joaquin Ruiz, Stephen E. Kesler, Adam Simon and John L. Muntean
Re-Os age of the Pueblo Viejo epithermal deposit, Dominican Republic
Economic Geology and the Bulletin of the Society of Economic Geologists (April 2014) 109 (2): 503-512

Abstract

Re-Os analyses of pyrite from the Pueblo Viejo high-sulfidation epithermal deposit (both Monte Negro and Moore ore zones) yield an isochron age of 111.9 + or - 3.7 Ma and initial (super 187) Os/ (super 188) Os ratio of 0.22 + or - 0.18 (mean square of weighted deviates = 84, n = 21). Isochrons grouped by pyrite setting (layered versus vein) or locations yield ages within uncertainty of the overall isochron and with each other and, as such, do not yield temporally distinguishable ages. Sphalerite vein samples as well as shale source rocks show evidence of open system behavior and loss of Re and therefore are not included in the above regression. These results confirm that the Pueblo Viejo deposit is Early Cretaceous in age and coeval with the volcanic Los Ranchos Formation, which hosts the deposit. Recent paleontological age assignments for the Hatillo Formation, which overlies the Los Ranchos Formation, show that it is only slightly younger, opening the possibility that mineralization in the Hatillo Formation could also be related to late stages of Los Ranchos magmatism. Whether these revised Los Ranchos-Hatillo relations provide sufficient cover to account for the paragenetically late formation of pyrophyllite at Pueblo Viejo remains unclear. Recognition that Pueblo Viejo is coeval with the Los Ranchos Formation shows that large-scale, high-sulfidation epithermal mineralization can form from basal island-arc tholeiitic magmatism. A review of available experimental data confirms that these magmas can generate hydrothermal solutions of the necessary composition; favorability of the Los Ranchos Formation might have been enhanced by its bimodal composition. These results suggest that exploration for epithermal precious metal deposits should include basal island-arc tholeiite terranes.


ISSN: 0361-0128
EISSN: 1554-0774
Coden: ECGLAL
Serial Title: Economic Geology and the Bulletin of the Society of Economic Geologists
Serial Volume: 109
Serial Issue: 2
Title: Re-Os age of the Pueblo Viejo epithermal deposit, Dominican Republic
Affiliation: University of Arizona, Department of Geosciences, Tucson, AZ, United States
Pages: 503-512
Published: 201404
Text Language: English
Publisher: Economic Geology Publishing Company, Lancaster, PA, United States
References: 56
Accession Number: 2014-004505
Categories: Economic geology, geology of ore depositsGeochronology
Document Type: Serial
Bibliographic Level: Analytic
Illustration Description: illus. incl. sect., 1 table, geol. sketch maps
N18°19'60" - N18°30'00", W70°49'60" - W70°40'00"
Secondary Affiliation: University of Michigan, USA, United StatesNevada Bureau of Mines and Geology, USA, United States
Country of Publication: United States
Secondary Affiliation: GeoRef, Copyright 2017, American Geosciences Institute. Abstract, Copyright, Society of Economic Geologists. Reference includes data from GeoScienceWorld, Alexandria, VA, United States
Update Code: 201404
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