ID-TIMS U–Pb geochronology at the 0.1‰ level using 1013 Ω resistors and simultaneous U and 18O/16O isotope ratio determination for accurate UO2 interference correction-Reference-Cited by-同舟云学术

ID-TIMS U–Pb geochronology at the 0.1‰ level using 1013 Ω resistors and simultaneous U and 18O/16O isotope ratio determination for accurate UO2 interference correction

Published:2017 Issue:3 Volume:32 Page:579-586
ISSN:0267-9477
Container-title:Journal of Analytical Atomic Spectrometry
language:en
Short-container-title:J. Anal. At. Spectrom.

Author:

Wotzlaw Jörn-Frederik¹²³⁴^ORCID,Buret Yannick¹²³⁴,Large Simon J. E.¹²³⁴,Szymanowski Dawid¹²³⁴^ORCID,von Quadt Albrecht¹²³⁴

Affiliation:

1. Institute of Geochemistry and Petrology

2. Department of Earth Sciences

3. ETH Zurich

4. Switzerland

Abstract

We document recent advances in analytical protocols that employ 10¹³ Ω resistors in the Faraday cup amplifier feedback loop for high-precision U–Pb geochronology by isotope dilution thermal ionisation mass spectrometry (ID-TIMS).

Publisher

Royal Society of Chemistry (RSC)

Subject

Spectroscopy,Analytical Chemistry

Link

http://pubs.rsc.org/en/content/articlepdf/2017/JA/C6JA00278A

Reference27 articles.

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5. Measurement of small ion beams by thermal ionisation mass spectrometry using new 1013Ohm resistors

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