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- W4254302512 abstract "Abstract. Cassiterite (SnO2) is the most common ore phase of Sn. Typically containing 1–100 µg/g U and relatively low concentrations of common Pb the mineral has been increasingly targeted for U-Pb geochronology, principally via micro-beam methods, to understand the timing and durations of granite related magmatic-hydrothermal systems throughout geological time. However, due to the extreme resistance of cassiterite to most forms of acid digestion, to date, there has been no published method permitting the complete, closed system decomposition of cassiterite under conditions where the basic necessities of measurement by isotope dilution can be met, leading to a paucity of reference, and validation materials. To address this a new low blank (" @default.
- W4254302512 created "2022-05-12" @default.
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- W4254302512 date "2020-01-16" @default.
- W4254302512 modified "2023-10-17" @default.
- W4254302512 title "High-precision ID-TIMS Cassiterite U-Pb systematics using a low-contamination hydrothermal decomposition: implications for LA-ICP-MS and ore deposit geochronology" @default.
- W4254302512 doi "https://doi.org/10.5194/gchron-2019-22" @default.
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