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• W2019400298 abstract "Many granites that occur in orogenic belts such as the Himalaya, the Hercynides or Caledonides are thought to result from anatexis of the lower parts of over-thickened thrust-stacked crustal units, just preceding termination of the orogenic cycle. Numerous Tertiary granitoids occur in the Rhodope Zone of northern Greece (and adjacent regions of Bulgaria), a belt regarded as an eastern extension of the Alpine System. These granites could also be regarded as syn- or late-tectonic crustal melts in that some have been emplaced as sheet-like bodies along major Alpine thrust planes, and show a strong marginal foliation parallel to the pervasive Alpine compressional fabrics. In detail, however, the geochemistry of the granitoids, their timing and relationships with country rocks, suggest they have been emplaced in an extensional regime that is related to the collapse of the Hellenic Orogen and, more particularly, to the crustal thinning that the Aegean region has suffered since the mid-Tertiary. Rather than being products of crustal thickening, it is suggested that their petrogenesis is related to the elevation of thermal gradients during the extensional phase, which initiated thermal breakdown of hydrous minerals in the lithosphere and lower crust that had existed metastably during compression and the subduction of cool ocean lithosphere beneath the region in the late Mesozoic-early Tertiary." @default.
• W2019400298 created "2016-06-24" @default.
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• W2019400298 date "1992-09-01" @default.
• W2019400298 modified "2023-09-27" @default.
• W2019400298 title "Tertiary granitoids of Rhodope, northern Greece: Magmatism related to extensional collapse of the Hellenic Orogen?" @default.
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• W2019400298 doi "https://doi.org/10.1016/0040-1951(92)90327-3" @default.
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