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The studied area is the North Dobrogea Orogen, Pricopan Massif. Compared to the other massive from the North Dobrogea, the Pricopan massif has a more rugged relief. The Pricopan massif is mostly a granite plutonic body with a lenticular shape, with the long axis (AL) oriented NNW-SSE and the transverse axis (AT). In the southern part, the Pricopan Massif is made up of diagenized sedimentary rocks, named the "Carapelit series". In the ridge area of the granite sector, there are alternations of peaks and saddles, st...

The North Dobrogean Orogen is located between the Sf Gheorghe fault to the north and Peceneaga -Camena to the south. Structurally, it involves four tectonic units with NW-SE direction: M?cin unit, Niculi?el unit, Consul unit and Tulcea unit. The M?cin unit comprise a large variety of rocks assemblage, including sedimentary rocks, metamorphic rocks and igneous rocks. All this rocks assemblage belongs to several subunits developed on quasi-parallel NW-SE direction. M?cin unit has been interpreted as nappe folded ove...

Several pots belonging to Neolithic cultures from the Romanian Plain contain crystals of brown hornblende. The brown hornblende is a calcic mineral belonging to the amphibole family, a highly complex series of inosilicates. Interestingly, the clay used as raw material for these Neolithic pots contains green, not brown, hornblende. No neighbouring sands (which could be added as a temper) contain such brown crystals. Therefore, the existence of the brown hornblende can be explained by in situ formation at the expens...