Age of the Peach Springs Tuff, southeastern California and western Arizona
Sanidine separates from pumice of the early Miocene Peach Springs Tuff are concordantly dated at 18.5??0.2 Ma by two isotopic techniques. The Peach Springs Tuff is the only known unit that can be correlated between isolated outcrops of Miocene strata from the central Mojave Desert of southeastern California to the western Colorado Plateau in Arizona, across five structural provinces, a distance of 350 km. Thus, the age of the Peach Springs Tuff is important to structural and paleogeographic reconstructions of a large region. -from Authors
Citation Information
Publication Year | 1990 |
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Title | Age of the Peach Springs Tuff, southeastern California and western Arizona |
Authors | J. E. Nielson, D. R. Lux, G. B. Dalrymple, A. F. Glazner |
Publication Type | Article |
Publication Subtype | Journal Article |
Series Title | Journal of Geophysical Research |
Index ID | 70016319 |
Record Source | USGS Publications Warehouse |