Direct evidence for the origin of low-18O silicic magmas: quenched samples of a magma chamber's partially-fused granitoid walls, Crater Lake, Oregon (Q281925): Difference between revisions
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Latest revision as of 18:56, 12 September 2024
Journal Article published in 1989
| Language | Label | Description | Also known as |
|---|---|---|---|
| English | Direct evidence for the origin of low-18O silicic magmas: quenched samples of a magma chamber's partially-fused granitoid walls, Crater Lake, Oregon |
Journal Article published in 1989 |
