A calcite reference material for LA‐ICP‐MS U‐Pb geochronology 论文

2017Geochemistry Geophysics Geosystems引用 494顶会
Geological and Geochemical AnalysisGeology and Paleoclimatology ResearchGeochemistry and Geologic Mapping

详细信息

发表期刊/会议
Geochemistry Geophysics Geosystems
发表日期
2017-05-30
发表年份
2017

关键词

Geological and Geochemical AnalysisGeology and Paleoclimatology ResearchGeochemistry and Geologic Mapping

摘要

Abstract U‐Pb dating of calcite is an emerging but rapidly growing field of application in geochronology with great potential to inform problems in landscape, basin, and mountain belt evolution, through age determination of diagenetic cements, vein mineralization, and geological formations difficult to date otherwise. In this brief, we present isotope dilution U‐Pb isotope measurements on a sample of calcite (WC‐1) that has been and will continue to be used as a reference material for in situ U‐Pb Laser Ablation Inductively Coupled Plasma Mass Spectrometry (LA‐ICP‐MS) dating, and which is suitable to be distributed to the geochronological community. We present in situ measurements using LA‐ICP‐MS to demonstrate the suitability of WC‐1 for use as a U‐Pb dating reference material, in spite of it not being isotopically homogeneous. The WC‐1 calcite sample is 254.4 ± 6.4 Ma old and comprised 85–98% radiogenic lead. It presents a suitable reference material that can facilitate dating of calcite ranging in age from Precambrian to late Neogene age.

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