Initial Characterisation ofSK01Sanidine: A Candidate40Ar/39ArReference Material

Author:

Li Youjuan12ORCID,Jicha Brian R.2,Zhang Wanfeng3,Chen Wen4,Singer Brad S.2,Zheng Dewen13,He Huaiyu56

Affiliation:

1. State Key Laboratory of Earthquake Dynamics, Institute of Geology, China Earthquake Administration Beijing 100029 China

2. Department of Geoscience University of Wisconsin‐Madison 1215 West Dayton Street Madison WI 53706 USA

3. State Key Laboratory of Isotope Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences Guangzhou 510640 China

4. Key Laboratory of Isotope Thermochronology, Key Laboratory of Deep Dynamic, Institute of Geology, Chinese Academy of Geological Sciences Beijing 100037 China

5. State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences Beijing 100029 China

6. College of Earth and Planetary Sciences University of Chinese Academy of Sciences Beijing 100049 China

Abstract

The precision and accuracy of40Ar/39Ar dates are ultimately linked to co‐irradiated reference materials of known age. Here we provide new data from the SK01 sanidine, which was analysed in three different laboratories to evaluate it as a40Ar/39Ar reference material. Aliquots of 5 mg, incrementally heated in two laboratories, yielded indistinguishable results with a weighted mean age of 27.58 ± 0.06 Ma (95% confidence level). Single‐crystal step heating and single‐crystal total fusion analyses of SK01 sanidine were undertaken in the third laboratory to further test the intracrystalline homogeneity. For the seven step‐heating analyses, six crystals yielded nearly concordant age spectra with40Ar/39Ar ages ranging from 26.853 ± 0.094 Ma to 26.963 ± 0.067 Ma, whereas one crystal gave an older age of 27.774 ± 0.071 Ma with a slightly discordant age spectrum. Twenty‐three single‐crystal total fusion analyses yielded40Ar/39Ar ages ranging from 27.070 ± 0.108 Ma to 27.736 ± 0.062 Ma with a dispersion of ~ 3.8%. The older ages from single‐crystal total fusion dates are interpreted to reflect an inherited or excess argon component in some crystals. This is an initial characterisation of the SK01 sanidine, and additional work needs to be conducted to further evaluate the age dispersion so that it can be utilised as a40Ar/39Ar reference material.

Funder

National Natural Science Foundation of China

Publisher

Wiley

Subject

Geochemistry and Petrology,Geology,Geochemistry and Petrology,Geology

Reference54 articles.

1. Incremental heating of Bishop Tuff sanidine reveals preeruptive radiogenic Ar and rapid remobilization from cold storage

2. 40Ar/39Ar and U–Pb dating of the Fish Canyon magmatic system, San Juan Volcanic field, Colorado: Evidence for an extended crystallization history

3. EARTHTIME: A community‐based effort towards high‐precision calibration of Earth history;Bowring S.A.;Geochimica et Cosmochimica Acta,2005

4. The Fish Canyon Tuff: A potential standard for the 40Ar/39Ar and fission‐track dating methods;Cebula G.T.;Terra Cognita,1986

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