Facies and paleogeography of the marine Upper Permian and of the Permian-Triassic boundary in the Southern Alps (Bellerophon formation, Tesero Horizon)

Author:

Noé Sibylle U.

Publisher

Springer Science and Business Media LLC

Subject

Paleontology,Stratigraphy,Geology

Reference98 articles.

1. ACCORDI, B. (1956): Calcareous algae from the Upper Permian of the Dolomites (Italy) with stratigraphy of the ‘Bellerophon-Zone’.—J. Paleont. Soc. India1, 75–84, 12 Pls., Lucknow

2. ADAMS, J.E. & RHODES, M.L. (1960): Dolomitization by seepage refluxion.—AAPG Bull.44, 1912–1920, 4 Figs., Tulsa

3. AIGNER, T. (1982): Calcareous tempestites: storm-dominated stratification in Upper Muschelkalk limestones (Middle Trias, SW-Germany).—In: EINSELE, G. & SEILACHER, A. (Eds.): Cyclic and event stratification, 180–198, 10 Figs., Berlin-Heidelberg-New York (Springer)

4. Lecture Notes in Earth Sciences;T. Aigner,1985

5. ASSERETO, R., BOSELLINI, A., SESTINI, F. & SWEET, W.C. (1973): The Permian-Triassic boundary in the Southern Alps (Italy).—In: LOGAN A.S. & HILLS, A.B. (eds.): The Permian and Triassic systems and their mutual boundary, 176–199, 6Figs., Calgary, Alberta

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