THE MEDITERRANEAN LOWER CRETACEOUS

•1- г
Fig. 27. Lithofacies map with sketches of the equal thicknesses and the palaeogeographic environments. Berriasian
(after P у с к о D а, H и к о л о в, 1984)
Lithofacies /чар: J — limestones; 2 - cla\o• limestones; 3—marls; 4 — marls with rare intercalations of siltstones; 5 — dolomites;
n"—sandstones; 7 — siltstones; H — conglomerates: 9 — i rcccia-ccnglomcratcs; JO—mixed rocks; //--spicules of Spongia;
12 — C;ilpionel'»diie; 13 — biodctrile; Ы — Alfac: 15 — investigated sections in outcrops; 16 •— investigated sections in drillings;
17 — lithological complexes with repeated rock types in the section; 76* — lithological complexes with pointed out basement and upper
part; 19 — boundary between the lithologie::I complexes; 20 — boundary between the lithological complexes in regions of total
denudation or dry land. Sketch of the cqi'al thicknesses (a): 21 — proved; 22 — probables. Sketch of the pafacogeowaphic environments
(b). Marine environments: 23 — shallow shelf—carbonates platform; 24 — deep shelf; 25 — flysch trough (comparatively deep-sea
sedimentation); Continental environments: 26 — mountain relief; 27— plate-like relief