Change from shallow to deep-water environment on an isolated carbonate platform in the Middle Triassic of the Transdanubian Range (Hungary)

Author:

Karádi Viktor,Budai Tamás,Haas János,Vörös Attila,Piros Olga,Dunkl István,Tóth Emőke

Funder

National Research, Development and Innovation Office

NKFIH

Universidad de Granada

Nemzeti Kutatási Fejlesztési és Innovációs Hivatal

Publisher

Elsevier BV

Subject

Paleontology,Earth-Surface Processes,Ecology, Evolution, Behavior and Systematics,Oceanography

Reference74 articles.

1. Ladinian/Carnian ammonoids and conodonts from the classic Schilpario – Pizzo Camino area (Lombardy): revaluation of the biostratigraphic support to chronostratigraphy and paleogeography;Balini;Riv. It. Paleont. Strat.,2000

2. Triassic ammonoid biostratigraphy: an overview;Balini,2010

3. Ostracoden aus paläozoischen pelagischen Kalken der karnischen Alpen (Silurium bis Unterkarbon);Bandel;Senckenb. Lethaea,1975

4. From rifting to drifting: tectonic evolution of the South-Alpine upper crust from the Triassic to the Early Cretaceous;Bertotti;Sediment. Geol.,1993

5. Conodonts from the Anisian-Ladinian succession of Bagolino, Brescian Prealps (Brescia, Lombardy, Northern Italy);Brack,1998

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