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Fig. 4 in The Berriasian-Valanginian And Aptian Deposits From The North-Western Part Of The Piatra Craiului Massif: Stratigraphic Relationships, Facies And Depositional Environments

Fig. 4 Stratigraphic logs of the A Padinile Frumoase succession; and the B Drumul lui Lehman succession. Legend: 1, massive limestone; 2, marly limestone; 3, allodapic limestone; 4, breccia; 5, conglomerate; ES, erosional surface; GRPC, Gura Râului Paraconglomerates; MB, monomictic breccia; MOC, monomictic orthoconglomerate; MPC, monomictic paraconglomerate; U, unconformity. M, W, P, G, R = mudstone, wackestone, packstone, grainstone, rudstone in Dunham's (1962) limestone classification. ristic for the Berriasian-Valanginian and Barremian- Steinmann (Fig. 8n), Carpathoporella occidentalis Aptian intervals. The Berriasian-Valanginian pebbles Dragastan (Fig. 8p), Coscinophragma cribrosa (Reuss) consist of a wide range of microfacies such as fenestral (Fig. 8s), and Lithocodium aggregatum Elliott (Fig. 8r). mudstone, peloidal bioclastic packstone or peloidal The limestone fragments-bearing monomictic breccia are bioclastic packstone/grainstone. The microfollowed by monomictic conglomerates, similarly rich in paleontological assemblage contains foraminifera limestone pebbles (Fig. 3c-e). Microfacies and [Ammobaculites sp., Montsalevia salevensis (Charollais, micropaleontological analysis has shown that, similar Brönnimann & Zaninetti) (Fig. 8), Meandrospira sp., with the breccia components, the most important Protopeneroplis ultragranulata (Gorbatchik), Pfenderina microfacies and microfossils of the pebbles are character- neocomiensis (Pfender)] and dasycladalean algae.