Oxygen and hydrogen isotope evidence for large-scale circulation and interaction between ground waters and igneous intrusions, with particular reference to the San Juan Volcanic Field, Colorado
The 33 to 25 m.y.-old intrusive and volcanic rocks from western San Juan Mountains (Silverton-Ouray area of Colorado) are all abnormally low in O¹⁸ relative to most igneous rocks, particularly along the eastern edge of the Silverton Caldera where the average δO¹⁸ = -5. The only exceptions to this ar...
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Other Authors: | , , , |
Format: | Book Part |
Language: | English |
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Carnegie Institution of Washington
1974
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Online Access: | https://authors.library.caltech.edu/117618/ https://authors.library.caltech.edu/117618/1/Taylor_1974p299.pdf https://resolver.caltech.edu/CaltechAUTHORS:20221027-145941066 |