摘要
The paper presents the results of the latest research carried out on calc-silicate rocks from Novo Selo - Kriva Lakavica, Eastern Macedonia. One hundred samples were collected for research. Chemical, optical and X-ray analyses were performed. The results show that the dominant material in these rocks is calcite. The following minerals were also present: diopside-hedenbergite, augite, actinolite, pargasite, K-feldspar, plagioclase, quartz, titanite, vesuvianite, clinozoisite, andradite-grossular, scapolite and prehnite. These mineral associations and the regional distribution of calc-silicate rocks from Novo Selo - Kriva Lakavica indicate regional metamorphic conditions of origin. Such mineral associations have been described in many regional metamorphic complexes.
- 出版日期2012