Naslov
Structural fabric of the metamorphosed rocks of tMt. Krndija and the eastern part of Mt. Papuk

Autori
Jamičić, Domagoj

Izvornik
Bulletin scientifique. Section A, Sciences naturelles, techniques et médicales. (0350-1558) 21 (1976), 1-2; 2-3

Vrsta, podvrsta i kategorija rada
Radovi u časopisima, članak, znanstveni

Ključne riječi
structural fabric; Krndija; Croatia

Sažetak
In the course of the geological mapping of the areas on Mt. Krndja and a part of Mt. Papuk, sheet Oraho-vica M 1:25000, a great many structural elements were collected, such as: strike and dip of foliation, lineations (corugation) and axis of the small folds, strike and dip of fissures. All these elements were used in making a structural diagrams which provided, besides an analysis of the geological rnap, some certain results and features of the crystalline schists fabric of the areas of Mt. Krndija and the eastern part of Mt. Pa-puk. According to an analysis of the data presented the mentioned areas could be structurally divided into two parts: a southern and a northern complex. The southern fabric is represented by a series of progressive metamorphic rocks which, in respect to our investigations, belong originally to the same series of geosynclinal sediments. This series is perforated in some places by small masses of granodiorites. The degree of metamorphism is increasing from the south to the north, and its sediments have metamorphosed to the grade which would correspond to the amphi-bole facies and partly to the fades of greenschists (according to Escola). This series is represented by granodiorites, gneiss, amphiboles, amphiboles schists, micaschists, quartzite and phyllites, with inserted pieces of graphite schists. Afterwards, this series was metamorphosed retrogradely, in some places up to the filonite degree.

Izvorni jezik
Engleski

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