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Based on the Bohemian Massif in the internal zone of the Variscides as case study, we present geological, geochemical, petrological and geochronological data arguing against a substantial mantle involvement in metamorphism and magma genesis in the area of the South Bohemian Batholith. In order to provide an alternative explanation consistent with heat transfer mechanism, we apply a two\u2010dimensional thermal\u2013kinematic modelling approach. The model calculates the transient lithospheric temperature field during crustal thickening and subsequent thinning by erosiorf from material parameters and boundary conditions specific to the study area. Model results show that the increased contribution of radiogenic heat in the thickened crust can indeed cause a substantial temperature increase in the middle and lower crust. Model predictions are in good agreement with observations, e.g. the\n            <jats:italic>P\u2013T\u2013t<\/jats:italic>\n            evolution of the country rocks, the formation of syn\u2010kinematic migmatites, the large volumes of peraluminous granites derived from dehydration melting of metasediments and the small volumes of lamprophyric melts from the mantle lithosphere. The results of this study emphasize the importance of radiogenic heat as the source for high\u2010temperature metamorphism and granite petrogenesis in the Bohemian Massif and potentially in other areas of the Variscan Orogen.\n          <\/jats:p>","DOI":"10.1144\/jgs.157.3.577","type":"journal-article","created":{"date-parts":[[2010,6,10]],"date-time":"2010-06-10T20:47:05Z","timestamp":1276202825000},"page":"577-587","update-policy":"https:\/\/doi.org\/10.1144\/crossmark-policy","source":"Crossref","is-referenced-by-count":171,"title":["Post\u2010collisional granite generation and HT\u2013LP metamorphism by radiogenic heating: the Variscan South Bohemian Batholith"],"prefix":"10.1144","volume":"157","author":[{"given":"A.","family":"GERDES","sequence":"first","affiliation":[{"name":"Geochemisches Institut, Goldschmidtstr. 1, 37077 G\u00f6ttingen, Germany"},{"name":"Departamento de Mineralog\u00eda y Petrolog\u00eda, Facultad de Ciencias, E\u201018002 Granada, Spain"},{"name":"Present address: NERC Isotope Geoscience Laboratory, Keyworth, Nottingham NG12 5GG, UK (e\u2010mail: )"}],"role":[{"vocabulary":"crossref","role":"author"}]},{"given":"G.","family":"W\u00d6RNER","sequence":"additional","affiliation":[{"name":"Geochemisches Institut, Goldschmidtstr. 1, 37077 G\u00f6ttingen, Germany"}],"role":[{"vocabulary":"crossref","role":"author"}]},{"given":"A.","family":"HENK","sequence":"additional","affiliation":[{"name":"Institut f\u00fcr Geologie, Pleicherwall 1, 97070 W\u00fcrzburg, Germany"}],"role":[{"vocabulary":"crossref","role":"author"}]}],"member":"1881","published-online":{"date-parts":[[2022,6,6]]},"reference":[{"key":"e_1_3_2_1_1","doi-asserted-by":"publisher","DOI":"10.1016\/0016-7037(91)90029-5"},{"key":"e_1_3_2_2_1","doi-asserted-by":"publisher","DOI":"10.1086\/314356"},{"key":"e_1_3_2_3_1","doi-asserted-by":"publisher","DOI":"10.1007\/BF00320902"},{"key":"e_1_3_2_4_1","doi-asserted-by":"publisher","DOI":"10.1093\/petrology\/32.2.365"},{"key":"e_1_3_2_5_1","doi-asserted-by":"publisher","DOI":"10.1029\/94JB02060"},{"key":"e_1_3_2_6_1","doi-asserted-by":"publisher","DOI":"10.1007\/s004100050308"},{"key":"e_1_3_2_7_1","doi-asserted-by":"publisher","DOI":"10.1126\/science.245.4922.1093"},{"key":"e_1_3_2_8_1","doi-asserted-by":"crossref","unstructured":"Blundell D. 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