Secondary ion mass spectrometry for the measurement of 232Th/230Th in volcanic rocks

被引:37
作者
Layne, GD [1 ]
Sims, KW [1 ]
机构
[1] Woods Hole Oceanog Inst, Woods Hole, MA 02543 USA
基金
美国国家科学基金会;
关键词
secondary ion mass spectrometry; ion microprobe; Th isotopes; U-series; U-Th disequilibrium;
D O I
10.1016/S1387-3806(00)00312-2
中图分类号
O64 [物理化学(理论化学)、化学物理学]; O56 [分子物理学、原子物理学];
学科分类号
070203 [原子与分子物理]; 070304 [物理化学]; 081704 [应用化学]; 1406 [纳米科学与工程];
摘要
A technique is presented for the determination of Th-232/Th-230 in volcanic rocks by secondary ion mass spectrometry (SIMS). The technique utilizes a large format high-resolution, high-transmission ion microprobe, the Cameca IMS 1270. Although samples of chemically separated Th are required. these samples demand no special treatment in addition to that already utilized in thermal ionization mass spectrometry. This SIMS technique has considerable advantages in terms of sample size requirement, ease of sample loading, and rapidity of analysis over existing techniques, while providing an overall reproducibility of 0.5%-1.0%. Replicates of standard reference materials and rock materials already characterized by other techniques show excellent agreement with established values, supporting the reliability and accuracy of this new method. (C) 2000 Elsevier Science B.V.
引用
收藏
页码:187 / 198
页数:12
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