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Digital-Desert :
Mojave Desert
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Mesozoic Rocks
Triassic PlutonsTriassic plutonic rocks are widely scattered in regions mostly west and southwest of the EMNSA (Barth and others, 1991; Miller, 1978). In the Clark Mountain area, several small dioritic stocks intrude Paleozoic strata, and one of these bodies has yielded K-Ar hornblende ages of 190 and 200 Ma (Burchfiel and Davis, 1971; Mueller and others, 1979). However, preliminary U-Pb zircon ages for these bodies are Late Jurassic (J.D. Walker, 1993, oral commun.). Evidently, the hornblende contained excess argon, resulting in ages spuriously old. No Triassic U-Pb ages have been reported for plutons in the EMNSA, but few candidates have been dated by U-Pb. A dioritic orthogneiss unit in the Granite Mountains, assigned a probable Triassic age by Howard and others (1987), is now known to be Jurassic (Young and others, 1992). Small bodies of hornblende monzonite, commonly present between the Teutonia batholith and septa of Paleozoic marble in the western New York Mountains, is similar to Triassic monzonites known in the western Mojave Desert. This hornblende monzonite is younger than Paleozoic rocks and older than the Early Cretaceous Mid Hills Adamellite. |
| Intro:: Nature:: Map:: Parks:: Points of Interest:: Ghosts & Gold:: Communities:: Roads & Trails:: People & History:: BLOG:: Weather:: :?:: glossary |
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Digital-Desert :
Mojave Desert
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Disclaimer: Some parts of this project were created with help from AI tools to fill in gaps or model historical patterns. Everything has been reviewed and fact-checked by real people to make sure it’s as accurate and useful as possible, though not every detail can be guaranteed. The goal is to offer solid starting points and unique niches for your own studies, exploration, and deeper research. These items are historical in scope and are intended for educational purposes only; they are not meant as an aid for travel planning. Copyright ©Walter Feller. 1995-2025 - All rights reserved. |