Lead and strontium isotopic evidence for crustal interaction and compositional zonation in the source regions of Pleistocene basaltic and rhyolitic magmas of the Coso volcanic field, California
- 1 January 1984
- journal article
- research article
- Published by Springer Nature in Contributions to Mineralogy and Petrology
- Vol. 85 (4) , 366-375
- https://doi.org/10.1007/bf01150293
Abstract
No abstract availableKeywords
This publication has 32 references indexed in Scilit:
- Magmatic inclusions in rhyolites, contaminated basalts, and compositional zonation beneath the Coso volcanic field, CaliforniaContributions to Mineralogy and Petrology, 1984
- Eruptive history of Mount Mazama and Crater Lake Caldera, Cascade Range, U.S.A.Journal of Volcanology and Geothermal Research, 1983
- Nd and Sr isotopic study of crustal and mantle inclusions from the Sierra Nevada and implications for batholith petrogenesisGSA Bulletin, 1983
- Lead and strontium isotopes and related trace elements as genetic tracers in the Upper Cenozoic rhyolite‐basalt association of the Yellowstone Plateau Volcanic FieldJournal of Geophysical Research, 1982
- Time-predictable bimodal volcanism in the Coso Range, CaliforniaGeology, 1982
- Pleistocene high‐silica rhyolites of the Coso Volcanic Field, Inyo County, CaliforniaJournal of Geophysical Research, 1981
- Trace element and isotopic effects of combined wallrock assimilation and fractional crystallizationEarth and Planetary Science Letters, 1981
- Heat flow in the Coso Geothermal Area, Inyo County, CaliforniaJournal of Geophysical Research, 1980
- Variations in Lead-Isotopic Compositions in Mesozoic Granitic Rocks of California: A Preliminary InvestigationGSA Bulletin, 1973
- Primitive and contaminated basalts from the Southern Rocky Mountains, U.S.A.Contributions to Mineralogy and Petrology, 1969