Re-evaluating genetic models for porphyry Mo mineralization at Questa, New Mexico: Implications for ore deposition following silicic ignimbrite eruption-Reference-Cited by-同舟云学术

Re-evaluating genetic models for porphyry Mo mineralization at Questa, New Mexico: Implications for ore deposition following silicic ignimbrite eruption

Published:2013-04 Issue:4 Volume:14 Page:787-805
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem. Geophys. Geosyst.

Author:

Rosera Joshua M.¹²,Coleman Drew S.¹,Stein Holly J.³⁴

Affiliation:

1. Department of Geological Sciences; University of North Carolina; Chapel Hill North Carolina USA

2. Chevron Mining Inc.; Questa New Mexico USA

3. AIRIE Program, Department of Geosciences; Colorado State University; Fort Collins Colorado USA

4. Physics of Geological Processes; University of Oslo; Oslo Norway

Funder

National Science Foundation

Geological Society of America

Sigma Xi Grants-in-Aid of Research

UNC Martin Fund

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

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4. Synthetic fluid inclusions. XVII. PVTX properties of high salinity H2O-NaCl solutions (> 30 wt % NaCl): Application to fluid inclusions that homogenize by halite disappearance from porphyry copper and other hydrothermal ore deposits;Becker;Econ. Geol.,2008

5. Oligocene caldera complex and calc-alkaline tuffs and lavas of the Indian Peak volcanic field, Nevada and Utah;Best;Geol. Soc. Am. Bull.,1989

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