The viability of leucite for 40Ar/39Ar dating and as a Quaternary standard

被引:5
作者
Karner, DB
Renne, PR
McDougall, I
Becker, T
机构
[1] Univ Calif Berkeley, Dept Geol & Geophys, Berkeley, CA 94720 USA
[2] Berkeley Geochronol Ctr, Berkeley, CA 94709 USA
[3] Australian Natl Univ, Res Sch Earth Sci, Canberra, ACT 0200, Australia
基金
美国国家科学基金会; 美国国家航空航天局;
关键词
geochronology; 40Ar/39Ar; standards; leucite; Italy;
D O I
10.1016/S0009-2541(00)00410-1
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 use of leucite (KAlSi2O6) as a 40Ar/39Ar dating standard has been avoided largely because of concerns over 40Ar(excess). Laser-fusion and resistance furnace step-heating 40Ar/39Ar analyses on leucite from a pyroclastic flow deposit from the Alban Hills are concordant and have atmospheric (40Ar/Ar-36 = 292.1 +/- 2.1 and 299.7 +/- 2.5, respectively) initial isotopic ratios. The error weighted mean 40Ar/39Ar ratio from step-heating and laser fusion data (N = 44) yields an age of 408 +/- 2 ka, including propagated errors in standards' isotopic ratios. The step-heating analysis indicates that leucite degasses at quite low temperatures (similar to 1100 degreesC), making it more suitable for K/Ar age analysis than sanidine. The mean and standard deviation from 10 potassium measurements by flame photometry and the error-weighted mean from five argon extractions produce a K/Ar age of 405 +/- 3 ka, in good agreement with the 40Ar/39Ar data and with precision comparable to several widely used primary K/Ar standards. This work suggests that leucite could become a very useful primary 40Ar/39Ar standard for dating Quaternary age rocks, thereby avoiding errors introduced by intercalibrating a Quaternary-age 40Ar/39Ar standard with a primary K/Ar standard. (C) 2001 Elsevier Science B.V. All rights reserved.
引用
收藏
页码:473 / 482
页数:10
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