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![Field photographs of the BBK succession. A) Exposure at the eastern coast of Kupinova cove (bedding planes of the key horizons are marked). B) Laminated and platy limestones of the Milna Formation and a single-fold slump of southern vergence (arrow). C) Sharp contact of the Milna laminites below and a slide block of skeletal–peloidal packstone above. D) Carbonate breccia of the disturbed upper part of the Milna Formation. E) Chaotic slump in the uppermost disturbed part of the Milna Formation. F) Sharp contact of the underlying chaotically folded laminite (chaotic slump) of the Milna Formation and the overlying calcispheric–microbioclastic wackestone–packstone of the Sveti Duh Formation.]()
![Photomicrographs of the microfacies and index fossils. A) Washed rudstone of the Cenomanian chondrodontid–rudist (Eoradiolites plicatus) facies of the Milna Formation from 2.0 m of the BBK section. B) Bioclastic–skeletal packstone–grainstone of the Milna Formation (on the left) and neptunian dike (on the right) with calcispheric–microbioclastic wackestone–packstone, intraclasts, and, lithoclasts of laminite from 1.5 m of the BBK section. C) Laminite with foraminifera characteristic of brackish conditions from 12.5 m of BBK section. D) Spirolina sp. from 12.5 m of the BBK section. E) Typical calcisphere wackestone of the Sveti Duh Formation with Whiteinella cf. baltica from 39.7 m of the BBK section. F) Late Cenomanian index microfossil Vidalina radoicicae from 35.7 m of the BBK section. G) Bioclastic wackestone with different sections of Heterohelix sp. cf. H. reussi from 75.0 m of the BSV section. H) Bioclastic wackestone with Saccocoma sp. from 26.05 m of the BSV section. I) Whiteinella cf. archaeocretacea from 18.75 m of the BSV section. J) Whiteinella cf. aprica from 22.55 m of the BSV section. K) Bio-lithoclastic packstone–grainstone and floatstone–rudstone with predominantly echinoderm fragments inserted in pelagic matrix (bioclastic wackestone) from 62.2 m of the BBK section. L) Scandonea samnitica from 87.6 m of the BSV section. M) Moncharmontia cf. compressa from 84.4 m of the BBK section.]()
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Sveti Duh Formation
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Journal Article
Response of a carbonate platform to the Cenomanian–Turonian Drowning and OAE 2: a case study from the Adriatic Platform (Dalmatia, Croatia) Available to Purchase
Journal: Journal of Sedimentary Research
Publisher: SEPM Society for Sedimentary Geology
Published: 01 March 2012
Journal of Sedimentary Research (2012) 82 (3): 163–176.
... to the Milna, Sveti Duh, and Gornji Humac formations ( Gušić and Jelaska 1990 ). The Milna Formation, of Cenomanian age, represents the oldest deposits on Brač. Carbonate facies in this formation include a variety of skeletal lithofacies (including rudists, other mollusks, and foraminifera) with common...
FIGURES
Image
Field photographs of the BBK succession. A) Exposure at the eastern coast... Available to Purchase
in Response of a carbonate platform to the Cenomanian–Turonian Drowning and OAE 2: a case study from the Adriatic Platform (Dalmatia, Croatia)
> Journal of Sedimentary Research
Published: 01 March 2012
) of the Milna Formation and the overlying calcispheric–microbioclastic wackestone–packstone of the Sveti Duh Formation.
Image
Photomicrographs of the microfacies and index fossils. A) Washed rudstone... Available to Purchase
in Response of a carbonate platform to the Cenomanian–Turonian Drowning and OAE 2: a case study from the Adriatic Platform (Dalmatia, Croatia)
> Journal of Sedimentary Research
Published: 01 March 2012
. E) Typical calcisphere wackestone of the Sveti Duh Formation with Whiteinella cf. baltica from 39.7 m of the BBK section. F) Late Cenomanian index microfossil Vidalina radoicicae from 35.7 m of the BBK section. G) Bioclastic wackestone with different sections of Heterohelix sp. cf. H. reussi
Journal Article
Upper Cretaceous Organic-Rich Laminated Limestones of the Adriatic Carbonate Platform, Island of Hvar, Croatia Available to Purchase
Journal: AAPG Bulletin
Publisher: American Association of Petroleum Geologists
Published: 01 August 1994
AAPG Bulletin (1994) 78 (8): 1313–1321.
... summary of the lithostratigraphy, according to Gušić and Jelaska (1990) , is as follows. Milna Formation (Cenomanian): platform interior, laminated facies, sporadically contains preserved organic matter. Sveti Duh Formation (lower Turonian): pelagic incursion over the platform. Gračišće...
FIGURES
