Controls of sea level fluctuations on the formation of Ordovician siliceous nodules in terrigenous offshore environments

Author:

Loi Alfredo,Dabard Marie-Pierre

Publisher

Elsevier BV

Subject

Stratigraphy,Geology

Reference53 articles.

1. Hydrothermal chert and associated siliceous rocks from the northern Pacific: their geological significance as indication of ocean ridge activity;Adachi;Sediment. Geol.,1986

2. Proximality trends in modern storm sands from the Helgoland Bight (North Sea) and their implications for basin analysis;Aigner;Senckenbergiana Marit.,1982

3. Geochemical constraints on the depositional setting of Palaeozoic cherts from the New England orogen, NSW, eastern Australia;Aitchison;Mar. Geol.,1990

4. La successione ordoviciano-siluriana inferiore nel Sarrabus (Sardegna sud orientale);Barca;Mem. Soc. Geol. Ital.,1979

5. Genesis and significance of the silico-aluminous nodules in the Ordovician of the Montagne Noire and the Massif Armoricain (France);Becq-Giraudon;Sediment. Geol.,1992

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