Hydrogen isotopic evidence of rhyolitic magma degassing during shallow intrusion and eruption
- 1 December 1983
- journal article
- research article
- Published by Springer Nature in Nature
- Vol. 306 (5943), 541-545
- https://doi.org/10.1038/306541a0
Abstract
No abstract availableKeywords
This publication has 24 references indexed in Scilit:
- Structure and emplacement of a rhyolitic obsidian flow: Little Glass Mountain, Medicine Lake Highland, northern CaliforniaGSA Bulletin, 1983
- Field gas chromatograph analyses of gases from a glowing dome at Merapi volcano, Java, Indonesia, 1977, 1978, 1979Journal of Volcanology and Geothermal Research, 1982
- Ion microprobe studies of water in silicate melts: Temperature-dependent water diffusion in obsidianEarth and Planetary Science Letters, 1982
- Magmatic volatiles in explosive rhyolitic eruptionsGeophysical Research Letters, 1981
- Diffusion in magmas at depth in the Earth: The effects of pressure and dissolved H2OEarth and Planetary Science Letters, 1981
- Ion microprobe studies of water in silicate melts. Concentration-dependent water diffusion in obsidianEarth and Planetary Science Letters, 1981
- Plinian-type eruptions in the medicine lake highland, california, and the nature of the underlying magmaJournal of Volcanology and Geothermal Research, 1978
- The Effects of Pressure, Temperature, and XH2Oon Phase Assemblage in Four Synthetic Rock CompositionsThe Journal of Geology, 1975
- Calculated Compaction Profiles of Rhyolitic Ash-Flow TuffsGSA Bulletin, 1973
- The variation of the deuterium content of natural waters in the hydrologic cycleReviews of Geophysics, 1964