2019
DOI: 10.2478/mipo-2019-0002
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Lamprophyric rock locations in Greece

Abstract: Twenty-four areas with lamprophyric formations have been located through a bibliographic search in Macedonia, Thrace, the islands and Attica. Most lamprophyre types have been identified including rare “alkali minette”. In most localities the dikes/sills appear to be late mantle products associated with deep faulting following extensional activity in granitoids.

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“…Hydrothermal fluids silicified the sandstones around the intrusion center and locally introduced finely disseminated pervasive sulfides (Fornadel et al, 2012). Late E-W striking dikes of shoshonitic composition crosscut the monzonite and other volcanic units (Voudouris, 2006;Kamvisis, 2019). The epithermal mineralization at Fakos is closely related to E-W trending fault zones (Figure 1B; Fornadel et al, 2012).…”
Section: Geological Overviewmentioning
confidence: 98%
“…Hydrothermal fluids silicified the sandstones around the intrusion center and locally introduced finely disseminated pervasive sulfides (Fornadel et al, 2012). Late E-W striking dikes of shoshonitic composition crosscut the monzonite and other volcanic units (Voudouris, 2006;Kamvisis, 2019). The epithermal mineralization at Fakos is closely related to E-W trending fault zones (Figure 1B; Fornadel et al, 2012).…”
Section: Geological Overviewmentioning
confidence: 98%