Wachowiak, J., Tobo³a, T., 2014. Phase tran si tions in the bo rate min er als from the K³odawa salt dome (cen tral Po land) as indi ca tors of tem per a ture pro cesses in salt diapirs. Geo log i cal Quar terly, 58 (3): 543-554, doi: 10.7306/gq.1170The diapiric struc tures of the Pol ish Low lands are tec toni cally deeply seated down to the autochthonous Zechstein strata at a depth of ca. 6 km. In the pro cess of deep burial and halokinetic diapirism, the salt rocks were sub jected to diagenetic and meta mor phic trans for ma tions, with the tem per a ture be ing an es sen tial fac tor. Con sid er ing the ther mal gra di ent, a tem per ature of up to ca. 200°C can be achieved in the salt dome within a depth range from sev eral hun dred metres to 6 km, which may lead to trans for ma tions of the ma jor ity of salt min er als. Phase tran si tions of two bo rate min er als -boracite and congolite from the K³odawa salt dome -pro vide ev i dence for higher tem per a tures in the salt dome rocks. The authigenic euhedral crys tals of those bo rate min er als dis play their ex ter nal habitus in am bi ent tem per a ture in the form of reg u lar sym me try (F43c -pseudo-reg u lar poly he drons), whereas their in ter nal struc ture is lower: orthorhombic (Pca2 1 ) for boracite and rhombohedral (R3 C ) for congolite. The heat ing and cool ing of boracite and congolite crys tals show re vers ible phase tran si tion. At a tem per a ture of ca. 270°C, boracite crys tals change their sym me try: orthorhombic « cu bic. In the case of congolite three revers ible phase tran si tions within a tem per a ture range of 50-339°C can be ob served: rhombohedral « monoclinic « orthorhombic « cu bic sym me try. Those phase tran si tions, con firmed ex per i men tally in our study, clearly doc u ment at least lo cal oc cur rences of tem per a tures ex ceed ing 339°C in the K³odawa salt dome.