On the Application of <sup>238</sup>U, <sup>235</sup>U, and <sup>232</sup>Th Decay Series Disequilibria to Understanding the Processes and Timescales of Oceanic Basalt Petrogenesis
Understanding how processes of magma genesis and magma differentiation control and modify the chemical composition of erupted lavas from the geochemical measurements of the latter is an under-constrained inverse problem, as there is only one known parameter—the measured composition of the erupted la...
Gorde:
| Egile Nagusiak: | , , , , , |
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| Formatua: | Artigo |
| Hizkuntza: | Inglês |
| Argitaratua: |
MDPI AG
2026-01-01
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| Saila: | Geosciences |
| Gaiak: | |
| Sarrera elektronikoa: | https://www.mdpi.com/2076-3263/16/1/34 |
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