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What is Geysers-Cobb Mountain Magma System Analysis about?
The study presents U-Pb isotopic ages for zircons from the Geysers Plutonic Complex, revealing that its crystallization occurred during the early Pleistocene, specifically between 1.1 and 1.8 million years ago. The results indicate that the main body of the complex was emplaced over a short time interval of approximately 0.2 million years, coinciding with the zircon crystallization ages of overlying volcanic units. This research contributes to understanding the thermal history and geological evolution of th
- Author
- Zefannya Mesakh
- Language
- EN