Controls of sea level fluctuations on the formation of Ordovician siliceous nodules in terrigenous offshore environments
- 1 November 2002
- journal article
- Published by Elsevier in Sedimentary Geology
- Vol. 153 (3-4) , 65-84
- https://doi.org/10.1016/s0037-0738(02)00102-1
Abstract
No abstract availableKeywords
This publication has 18 references indexed in Scilit:
- Hydrothermal chert and associated siliceous rocks from the northern Pacific their geological significance as indication od ocean ridge activityPublished by Elsevier ,2003
- Silica diagenesis in Eocene shallow‐water platform carbonates, southern PyreneesSedimentology, 1999
- Upper Middle Devonian (Givetian) gastropods from the Kersadiou Formation, Brittany, FranceJournal of Paleontology, 1999
- Early diagenesis: impact of organic matter on mass physical properties and processes, California continental marginMarine Geology, 1999
- Pure siliceous ooze, a diagenetic environment for early chert formationGeology, 1994
- Shell beds as tools in basin analysis: the Jurassic of Kachchh, western IndiaJournal of the Geological Society, 1993
- Genesis and significance of the silico-aluminous nodules in the Ordovician of the Montagne Noire and the Massif Armoricain (France)Sedimentary Geology, 1992
- Low-temperature opal-CT precipitation in Antarctic deep-sea sediments: evidence from oxygen isotopesEarth and Planetary Science Letters, 1991
- Geochemical constraints on the depositional setting of Palaeozoic cherts from the New England orogen, NSW, eastern AustraliaMarine Geology, 1990
- Biogenic chert in the Cow Head Group (Cambro‐Ordovician), western NewfoundlandSedimentology, 1987