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Map-scale folding and thrust faulting in Eocene flysch sediments (The Bay of Omiš) (CROSBI ID 89432)

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Tomljenović, Bruno Map-scale folding and thrust faulting in Eocene flysch sediments (The Bay of Omiš) // Vijesti Hrvatskoga geološkog društva, 37 (2000), 2; 106-108-x

Podaci o odgovornosti

Tomljenović, Bruno

engleski

Map-scale folding and thrust faulting in Eocene flysch sediments (The Bay of Omiš)

Outcrop- to map-scale structures in Eocene flysch sediments are studied in abandoned quarry in the Bay of Omiš, located in partly eroded hinge zone of a map-scale, Nw-plunging and SW-verging anticline. The folding was accompanied by thrust faulting, observed both in anticline core and its limbs. Structural data obtained from folds and faults suggest that observed structures accommodated NNE-SSW directed shortening during the Middle-Late Eocene deformational event.

faulting; folding; Extrernal Dinarides; Eocene flysch

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Podaci o izdanju

37 (2)

2000.

106-108-x

objavljeno

1330-1357

Povezanost rada

Rudarstvo, nafta i geološko inženjerstvo