1980
DOI: 10.1016/s0305-4403(80)80008-2
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Composition of iron age fine ceramics from Châtillon-s-Glâne (Kt. Fribourg, Switzerland) and the Heuneburg (Kr. Sigmaringen, West Germany)

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“…According to Maggetti and Kahr (1981) the above cited data depends mainly on five factors: (1) amount of temper in the sherds, (2) firing temperature, (3) initial grain size distribution of the clay, (4) clay mineralogy respectively chemistry, (5) firing atmosphere. As will be developed in section 5, the firing conditions and temperatures must have been identical for both ceramics; the chemical and mineralogical behaviour are very similar too (Maggetti and Galetti (1980). So the decisive factors are the temper and the clay grain size distribution.…”
Section: S H E R D C O L O U Rmentioning
confidence: 99%
“…According to Maggetti and Kahr (1981) the above cited data depends mainly on five factors: (1) amount of temper in the sherds, (2) firing temperature, (3) initial grain size distribution of the clay, (4) clay mineralogy respectively chemistry, (5) firing atmosphere. As will be developed in section 5, the firing conditions and temperatures must have been identical for both ceramics; the chemical and mineralogical behaviour are very similar too (Maggetti and Galetti (1980). So the decisive factors are the temper and the clay grain size distribution.…”
Section: S H E R D C O L O U Rmentioning
confidence: 99%