The 210 degreesC thermoluminescence (TL) peak of quartz, extracted from bri
ck fragments of Somero sacristy (Finland), which were partly elements of co
nstruction, were used for the measurement of archaeological dose for the pu
rpose of dating. The annual gamma dose-rate with cosmic component and beta
dose rate of bricks were measured using two types of TLD detectors (AL(2)O(
3)-C) inserted in situ and in laboratory, respectively, The improvements in
the precision of the TL measurements, components of annual dose assessment
are described, and the results of TL age determination are discussed and c
ompared with the archaeologically expected age. (C) 2000 Elsevier Science L
td. All rights reserved.