Primary versus diagenetic bedding in the limestone-marl/shale alternations of the epeiric seas, an example from the Lower Lias (early Jurassic) of SW Britain

Author:

Arzani Nasser

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology

Reference50 articles.

1. ARTHUR, M.A. and DEAN, W.E., 1991, A holistic geochemical approach to cyclomania: examples from Cretaceous pelagic sequences,In G. Einsele, W. Ricken, and A. Seilacher, eds., Cycles and Events in Stratigraphy. Springer-Verlag, Berlin, p. 126–166.

2. ARZANI, N., 1997, Facies and sedimentology at the Triassic-Jurassic boundary in SW Britain. Ph.D. thesis, University of Reading unpublished, 381 p.

3. ARZANI, N., 2004, Diagenetic evolution of mudstones: black shales to laminated limestones, an example from the Lower Jurassic of SW Britain:Journal of Science, Islamic Republic of Iran, v. 15, p. 257–267.

4. ASTIN, T.R. and SCOTCHMAN, I.C., 1988, The diagenetic history of some septarian concretions from the Kimmeridge Clay, England:Sedimentology, v. 35, p. 349–368.

5. BATHURST, R.G.C., 1975, Carbonate sediments and their diagenesis. Elsevier, Amsterdam, 658 p.

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