Articles | Volume 2, issue 2
https://doi.org/10.5194/gchron-2-425-2020
https://doi.org/10.5194/gchron-2-425-2020
Research article
 | 
18 Dec 2020
Research article |  | 18 Dec 2020

High-precision ID-TIMS cassiterite U–Pb systematics using a low-contamination hydrothermal decomposition: implications for LA-ICP-MS and ore deposit geochronology

Simon Tapster and Joshua W. G. Bright

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Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Publish subject to revisions (further review by editor and referees) (26 May 2020) by Brenhin Keller
AR by Simon Tapster on behalf of the Authors (01 Jun 2020)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (15 Jun 2020) by Brenhin Keller
RR by Gavin Piccione (29 Jun 2020)
RR by Corey Wall (06 Jul 2020)
ED: Publish subject to technical corrections (07 Jul 2020) by Brenhin Keller
ED: Publish subject to technical corrections (08 Jul 2020) by Klaus Mezger (Editor)
AR by Simon Tapster on behalf of the Authors (14 Jul 2020)  Manuscript 
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Short summary
Cassiterite is the primary tin ore mineral and is associated with other elements needed for green technology. The mineral is deposited from hydrothermal fluids released from magmas. Because it is extremely acid resistant, there has been difficulty dissolving the mineral for isotopic analysis. To improve the understanding of the timing and models of formation processes, we use a novel method to dissolve and extract radiogenic isotopes of the uranium-to-lead decay scheme from cassiterite.