Abstract
In situ-produced cosmogenic 10Be and 26Al measurements are widely applied in geomorphological studies and in archaeology and paleoanthropology as a chronologic tool applicable to the past 5 Ma. While most of these measurements are made from concentrates of quartz, a ubiquitous and resistant mineral, it is of great interest to extend this method to other silicates and particularly to the amorphous silicates whose purification may not be as straightforward. This paper presents a cleaning procedure that has been applied on ten samples of various siliceous rocks (chert, granite and quartzolite). The aim is to monitor the 10Be, 27Al and 26Al concentration evolution as a function of cleaning steps. While this protocol appears suitable for 10Be, when measuring 26Al careful attention should be paid to 27Al, whose concentration should be measured regularly to ensure that a constant value is achieved and most important, allowing measuring 26Al/27Al by AMS.
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