Stratigraphy and Tectonic Relationships Along the Senj - Ogulin Profile (Velika Kapela Mt., Croatia)
Abstrak
<div>Twelve lithostratigraphic units, representing a 5 km thick succession,</div><div>have been determined from the Senj -Ogulin profile through the</div><div>Velika Kapela Mt. This 45 km long sequence lies approximately normal</div><div>to the Dinaric strike. Carbonate deposits ranging from the Middle</div><div>Liassic to the Albian include laterally variable environments during</div><div>the Kimmeridgian and Lower Tithonian. The deposits were deformed</div><div>by compressive tectonics during the Tertiary tectonic cycle, and were</div><div>consequently reshaped by weaker Neotectonic transpression. Therefore</div><div>structures with the N-S strike, which are different to the common</div><div>Dinaric strike (NW-SE), are interpreted as a consequence of syngenetic bending during the Tertiary cycle, rather than rotation during the</div><div>Neotectonic cycle.</div>
Topik & Kata Kunci
Penulis (5)
Dubravko Matičec
Igor Vlahović
Ladislav Fuček
Nenad Oštrić
Ivo Velić
Akses Cepat
- Tahun Terbit
- 2010
- Sumber Database
- DOAJ
- DOI
- 10.4154/GC.1997.34
- Akses
- Open Access ✓