Oxygen isotopic investigation of silicic magmatism in the Stillwater caldera complex, Nevada: Generation of large-volume, low-δ18O rhyolitic tuffs and assessment of their regional context in the Great Basin of the western United States-Reference-Cited by-同舟云学术

Oxygen isotopic investigation of silicic magmatism in the Stillwater caldera complex, Nevada: Generation of large-volume, low-δ18O rhyolitic tuffs and assessment of their regional context in the Great Basin of the western United States

Published:2019-02-14 Issue:7-8 Volume:131 Page:1133-1156
ISSN:0016-7606
Container-title:GSA Bulletin
language:en
Short-container-title:

Author:

Watts Kathryn E.¹,John David A.¹,Colgan Joseph P.²,Henry Christopher D.³,Bindeman Ilya N.⁴,Valley John W.⁵

Affiliation:

1. U.S. Geological Survey, Menlo Park, California 94025, USA

2. U.S. Geological Survey, Denver, Colorado 80225, USA

3. Nevada Bureau of Mines and Geology, Reno, Nevada 89557, USA

4. Department of Earth Sciences, University of Oregon, Eugene, Oregon 97403, USA

5. Department of Geoscience, University of Wisconsin–Madison, Madison, Wisconsin 53706, USA

Publisher

Geological Society of America

Subject

Geology

Link

https://pubs.geoscienceworld.org/gsa/gsabulletin/article-pdf/131/7-8/1133/4729506/1133.pdf

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3. Coupled elemental and isotopic analyses of polygenetic zircons from granitic rocks by ion microprobe, with implications for melt evolution and the sources of granitic magmas;Barth;Chemical Geology,2010

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