Transition from marine to hypersaline conditions in the Messinian Tripoli Formation from the marginal areas of the central Sicilian Basin

Author:

Bellanca A,Caruso A,Ferruzza G,Neri R,Rouchy J.M,Sprovieri M,Blanc-Valleron M.M

Publisher

Elsevier BV

Subject

Stratigraphy,Geology

Reference49 articles.

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2. Carbonate preservation and climatic changes in the central Red Sea during the last 380kyr as recorded by pteropods;Almogi-Labin;Mar. Micropaleontol.,1998

3. Carbon isotopic evidence for the origin of a banded iron-formation in western Australia;Becker;Geochim. Cosmochim. Acta,1972

4. Evaporite carbonate cycles of the Messinian, Sicily: stable isotopes, mineralogy, textural features, and environmental implications;Bellanca;J. Sediment. Petrol.,1986

5. Isotope geochemistry, petrology and depositional environments of the diatomite-dominated Tripoli Formation (Lower Messinian), Sicily;Bellanca;Sedimentology,1986

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