散步 发表于 2025-3-27 00:33:26
https://doi.org/10.1007/978-88-470-1929-4inental crust relative to the mantle. The isotopic composition of boron in crystalline rocks of the continental crust (e.g., metamorphic and igneous lithologies) varies over a wide range of −20 to +10‰, depending on the B-isotope composition of the protoliths and on fractionation effects caused by p敬礼 发表于 2025-3-27 01:41:32
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Boron Isotope Analysis of Geological Materials,o include other materials with low B concentrations (e.g., carbonates, basaltic glass). The accurate and precise determination of the boron isotopic composition of geological materials is however a difficult task, particularly for those where boron is present in low-concentration. For solution metho反复拉紧 发表于 2025-3-27 16:40:39
,Boron Isotope Fractionation Among Vapor–Liquids–Solids–Melts: Experiments and Atomistic Modeling,al tracers of any vapor-, liquid- or melt-mediated process in the Earth’s interior. Feedback between experiments and computational predictions are required to gain insight into the processes driving isotope partitioning. This chapter comprises methods and results of selected experimental studies andPlaque 发表于 2025-3-27 20:34:52
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Boron Isotopes in the Ocean Floor Realm and the Mantle,cean island basalts and their implications for the B isotopic composition of the mantle. The chapter further discusses the B isotopic effects of assimilation of altered crustal materials in mantle-derived magmas. The systematics of seawater alteration on oceanic rocks are discussed, including sedime