Estimating the distribution of strontium isotope ratios ( 87 Sr/ 86 Sr) in the Precambrian of Finland

IF 1.3 4区 地球科学 Q2 GEOLOGY Bulletin of the Geological Society of Finland Pub Date : 2011-12-01 DOI:10.17741/BGSF/83.2.002
L. Kaislaniemi
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引用次数: 13

Abstract

A method to estimate the 87Sr/86Sr ratio of a rock based on its age and Rb/Sr ratio is presented. This method, together with data from the Rock Geochemical Database of Finland (n=6544) is used to estimate the 87Sr/86Sr ratios in the Precambrian of Finland and in its different major units. A generalization to cover the whole area of Finland is achieved by smoothing of estimation points. The estimation method is evaluated by comparing its results to published Rb-Sr isotope analyses (n=138) obtained on the Finnish Precambrian. The results show correspondence to different geological units of Finland, but no systematic difference between Archaean and younger areas is evident. Evaluation of the method shows that most of the estimates are reliable and accurate to be used as background material for provenance studies in archaeology, paleontology and sedimentology. However, some granitic rocks may have large (>1.0 %) relative errors. Strontium concentration weighted average of the estimates differs only by 0.001 from the average 87Sr/86Sr ratio (0.730) of the rivers on the Fennoscandian shield.
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芬兰前寒武纪锶同位素比值(87 Sr/ 86 Sr)分布的估算
提出了一种根据岩石年龄和Rb/Sr比值估算岩石87Sr/86Sr比值的方法。结合芬兰岩石地球化学数据库(n=6544)的数据,利用该方法估算了芬兰前寒武纪及其不同主要单元的87Sr/86Sr比值。通过对估计点进行平滑处理,实现覆盖整个芬兰地区的概化。将估算方法的结果与已发表的芬兰前寒武纪Rb-Sr同位素分析结果(n=138)进行了比较。结果显示芬兰不同地质单元的对应关系,但太古宙与更年轻地区的系统差异不明显。对该方法的评价表明,大多数估算值可靠、准确,可作为考古学、古生物学和沉积学物源研究的背景资料。然而,有些花岗质岩石可能有较大的相对误差(约1.0%)。估算的锶浓度加权平均值与Fennoscandian地盾上河流的平均87Sr/86Sr比值(0.730)仅相差0.001。
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来源期刊
CiteScore
1.30
自引率
0.00%
发文量
5
审稿时长
>12 weeks
期刊介绍: Bulletin of the Geological Society of Finland (BGSF) publishes research articles and short communications in all branches of geosciences. Contributions from outside Finland are welcome, provided that they contain material relevant to Finnish geology or are of general interest.
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