Discontinuity surfaces recorded in shallow-marine platform carbonates: an example from the Early Jurassic of the Velebit Mt. (Croatia)

Author:

Martinuš Maja,Bucković Damir,Kukoč Duje

Publisher

Springer Science and Business Media LLC

Subject

Paleontology,Stratigraphy,Geology

Reference80 articles.

1. Barattolo F, Romano R (2005) Shallow carbonate platform bioevents during the Upper Triassic-Lower Jurassic: an evolutive interpretation. Boll Soc Geol Ital 124:123–142

2. Bassoullet JP (1997) Les grands foraminifères. In: Cariou E, Hantzpergue P (eds) Biostratigraphie du jurassique ouest—européen et méditerranéen. Zonation parallèles et distribution des invertébrés et microfossiles. Bull Centre Rech Explor Prod Elf Mém 17:293–304

3. Bathurst RGC (1994) Carbonate sediments and their diagenesis. Developments in Sedimentology 12. Elsevier Science, Amsterdam, p 658

4. Bernoulli D, Jenkyns HC (1974) Alpine, Mediterranean and central Atlantic Mesozoic facies in relation to the early evolution of Tethys. In: Dott RH, Shaver RH (eds), Modern and ancient geosynclinal sedimentation. SEPM Spec Publ 18:129–160

5. Bortolotti V, Principi G (2005) Tethyan ophiolites and Pangea break-up. The Island Arc 14:442–470

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