Laser ablation inductively coupled plasma mass spectrometry (LA-ICP-MS) U–Pb carbonate geochronology: strategies, progress, and limitations
Laser ablation inductively coupled plasma mass spectrometry (LA-ICP-MS) U–Pb carbonate geochronology: strategies, progress, and limitations
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DOI:
10.5194/gchron-2-33-2020
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发表时间:
2020-04
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通讯作者:
N. Roberts;K. Drost;M. Horstwood;D. Condon;D. Chew;H. Drake;A. Milodowski;N. McLean;A. Smye;R. Walker;R. Haslam;K. Hodson;J. Imber;N. Beaudoin;JackKieran Lee
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作者:
N. Roberts;K. Drost;M. Horstwood;D. Condon;D. Chew;H. Drake;A. Milodowski;N. McLean;A. Smye;R. Walker;R. Haslam;K. Hodson;J. Imber;N. Beaudoin;JackKieran Lee
Abstract. Laser ablation inductively coupled plasma mass spectrometry (LA-ICP-MS) U–Pb geochronology of carbonate minerals, calcite in particular, is rapidly gaining popularity as an absolute dating method. The high spatial resolution of LA-ICP-MS U–Pb carbonate geochronology has benefits over traditional isotope dilution methods, particularly for diagenetic and hydrothermal calcite, because uranium and lead are heterogeneously distributed on the sub-millimetre scale. At the same time, this can provide limitations to the method, as locating zones of radiogenic lead can be time-consuming and “hit or miss”. Here, we present strategies for dating carbonates with in situ techniques, through imaging and petrographic techniques to data interpretation; our examples are drawn from the dating of fracture-filling calcite, but our discussion is relevant to all carbonate applications. We review several limitations to the method, including open-system behaviour, variable initial-lead compositions, and U–daughter disequilibrium. We also discuss two approaches to data collection: traditional spot analyses guided by petrographic and elemental imaging and image-based dating that utilises LA-ICP-MS elemental and isotopic map data.