Open AccessHigh‐resolution 40 Ar/ 39 Ar dating using a mechanical sample transfer system combined with a high‐temperature cell for step heating experiments and a multicollector ARGUS noble gas mass spectrometer
Author(s) -
Pfänder Jörg A.,
Sperner Blanka,
Ratschbacher Lothar,
Fischer Albrecht,
Meyer Martin,
Leistner Martin,
Schaeben Helmut
Publication year - 2014
Publication title -
geochemistry, geophysics, geosystems
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.928
H-Index - 136
ISSN - 1525-2027
DOI - 10.1002/2014gc005289
Subject(s) - analytical chemistry (journal) , silicate , mineralogy , quartz , crucible (geodemography) , materials science , geology , chemistry , metallurgy , organic chemistry , chromatography , computational chemistry
40 Ar/ 39 Ar dating of young (<1 Ma) and/or low potassium samples requires degassing of large amounts of material either by a laser or a furnace. A furnace excels in precise and reproducible temperature control and in providing a homogeneous temperature distribution even for relatively large sample amounts. For most systems, however, the degassed mineral or whole‐rock residues remain in the crucible after measurement. This reduces the thermal conductivity and increases the blank levels and baking times. To mitigate these problems, we combined a mechanical sample transfer system with a low volume (∼90 mL) high‐temperature cell. The system operates under ultrahigh vacuum and uses Mo‐crucibles, in which up to 1000 mg of sample is transferred into the furnace and taken out after degassing. The system has short baking times (20–30 min), highly reproducible heating conditions and an overall low blank level due to the absence of silicate (glassy) sample residue in the main crucible of the furnace. The system interconnects through a gas purification line with a low volume, high sensitivity multicollector ARGUS noble gas mass spectrometer. Intraday reproducibility of 40 Ar/ 36 Ar ratios measured on air aliquots of >5 × 10 −16 mol 36 Ar is better than 0.5‰–1.0‰ (1σ, n = 4–8). We illustrate the system performance by 40 Ar/ 39 Ar dating of whole‐rock samples and mineral separates from the Oman ophiolite as well as from the Siebengebirge, Heldburg, and Rhön volcanic provinces in Central Germany.