YBCs sanidine: A new standard for 40Ar/39Ar dating

被引:26
|
作者
Wang, Fei [1 ]
Jourdan, Fred [2 ,3 ]
Lo, Ching-Hua [4 ]
Nomade, Sebastien [5 ]
Guillou, Herve [5 ]
Zhu, Rixiang [1 ]
Yang, Liekun [1 ]
Shi, Wenbei [1 ]
Feng, Huile [1 ]
Wu, Lin [1 ]
Sang, Haiqing [1 ]
机构
[1] Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China
[2] Curtin Univ, JdL Ctr, Perth, WA 6845, Australia
[3] Curtin Univ, Dept Appl Geol, Perth, WA 6845, Australia
[4] Natl Taiwan Univ, Dept Geosci, Taipei 106, Taiwan
[5] LSCE, F-91198 Gif Sur Yvette, France
关键词
40Ar/39Ar geochronology; New standard; YBCs sanidine; FISH CANYON SANIDINE; INTERCALIBRATION; AGE; GEOCHRONOLOGY; CALIBRATION; EVOLUTION; ARGON; REDETERMINATION; ABUNDANCES; QIANGTANG;
D O I
10.1016/j.chemgeo.2014.09.003
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
The 40Ar/39Ar dating technique is based on neutron fluence monitors (standards). Recent investigation demonstrates that currently used standards are not as homogenous as believed and new standards are needed (Philips andMatchan, 2013). In this study, we report a newsanidine standard, YBCs, collected froma phonolite at Yabachi in Tibet, China, for single-grain 40Ar/39Ar dating. Aliquots were distributed to four international laboratories for analysis and intercalibration. The results show that YBCs crystals are homogenous in K content, 40Ar*/(39)A(Gamma K) (F-value) and age at the single grain level. The standard deviations of the F-value and age have small ranges from 0.29% to 0.53% and from 0.42% to 0.52%, respectively. These show that YBCs is a suitable standard for 40Ar/39Ar geochronology. The calibrated age of YBCs is 29.286 +/- 0.206 Ma, or neglecting the error in the decay constant, 29.286 +/- 0.045 Ma. Finally, the intercalibration factors (which allow direct comparison between standards) between YBCs and FCs, GA1550, ACs and HB3gr are calculated as: R-FCs(YBCs) = 1.044296 +/- 0.003968, R-GA1550(YBCs) = 0.291261 +/- 0.001148 R-ACs(YBCs) = 24.443066 +/- 0.068432 and R-HB3gr(YBCs) = 0.020312 +/- 0.000885. These values can be used to compare YBCs with other standards directly. (C) 2014 Elsevier B.V. All rights reserved. The 40Ar/39Ar dating technique is based on neutron fluence monitors (standards). Recent investigation demonstrates that currently used standards are not as homogenous as believed and new standards are needed (Philips andMatchan, 2013). In this study, we report a newsanidine standard, YBCs, collected froma phonolite at Yabachi in Tibet, China, for single-grain 40Ar/39Ar dating. Aliquots were distributed to four international laboratories for analysis and intercalibration. The results show that YBCs crystals are homogenous in K content, 40Ar*/(39)A(Gamma K) (F-value) and age at the single grain level. The standard deviations of the F-value and age have small ranges from 0.29% to 0.53% and from 0.42% to 0.52%, respectively. These show that YBCs is a suitable standard for 40Ar/39Ar geochronology. The calibrated age of YBCs is 29.286 +/- 0.206 Ma, or neglecting the error in the decay constant, 29.286 +/- 0.045 Ma. Finally, the intercalibration factors (which allow direct comparison between standards) between YBCs and FCs, GA1550, ACs and HB3gr are calculated as: R-FCs(YBCs) = 1.044296 +/- 0.003968, R-GA1550(YBCs) = 0.291261 +/- 0.001148 R-ACs(YBCs) = 24.443066 +/- 0.068432 and R-HB3gr(YBCs) = 0.020312 +/- 0.000885. These values can be used to compare YBCs with other standards directly. (C) 2014 Elsevier B.V. All rights reserved.
引用
收藏
页码:87 / 97
页数:11
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