In situ oxygen isotopes

LD Luigi Dallai
GB Gianluca Bianchini
RA Riccardo Avanzinelli
ED Etienne Deloule
CN Claudio Natali
MG Mario Gaeta
AC Andrea Cavallo
SC Sandro Conticelli
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In situ oxygen isotope analyses were performed using a CAMECA IMS 1280 HR2 ion microprobe at Centre de Recherches Pétrographiques et Géochimiques (CRPG, UMR 5873 CNRS-Université de Lorraine, Vandoeuvre les Nancy, France). The Cs+ primary ions beam of 2.5 nA were focused on a 10 µm diameter area and the electron gun used for the charge compensation. The negative secondary ions were measured with a mass resolution of 5000 (M/∆M) with an energy slit of 30 eV. Before each measurement, the sample was pre-sputtered for 90 s with a beam rastering on 15 µm to clean up the sample surface, then the secondary beam was automatically centred in the field aperture and contrast aperture and a beam rastering of 10 µm applied. The measurements are made on multicollection FC mode with counting time of 150 s. The instrumental mass fractionation was determined on the reference Bresil and Sonar 2. Bresil and Sonar 2 are two reference Quartz used two set up the instruments. The unknowns are normalized to Sonar 2, the external errors on the two sets of 5 and 7 measurements on Sonar 2 is 0.24‰, compared to 0.14‰ and 0.21‰ for each set of measurements. No time draft correction has been applied, as it does not significantly improve the precision of the measurements when the standards are not on the same holder than the samples. The internal errors on Standard and unknown range from 0.06 to 0.15‰. The secondary ion intensity relative to primary ion on samples is 80–100 % of the ones measured of standards, but there is no correlation between the secondary ion intensities and the δ18O, indicating a possible bias. The IMF correction is 6.35‰.

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