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 (Q282780): Difference between revisions
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Latest revision as of 18:58, 12 September 2024
Journal Article published in 2019
| Language | Label | Description | Also known as |
|---|---|---|---|
| English | 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 |
Journal Article published in 2019 |
