Covariance of C- and O-isotopes with magnetic susceptibility as a result of burial diagenesis of sandstones and carbonates: an example from the Lower Devonian La Vid Group, Cantabrian Zone, NW Spain

Author:

Schneider J.,Bechst�dt T.,Machel H. G.

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences

Reference57 articles.

1. Ala D (1996) High-resolution isotope stratigraphy of the Lower Devonian. Unpublished MS Thesis, University of Ottawa, Ottawa, pp 1?159

2. Alonso JL, Suárez Rodriguez A, Rodriguez Fernández LR, Farias P, Villegas F (1991) Mapa Geológico: La Pola de Gordón. 1:50.000 IGME, Madrid

3. Auclair AC, Joachimski MM, Lécuyer C (2003) Deciphering kinetic, metabolic and environmental controls on stable isotope fractionations between seawater and the shell of Terebratalia transversa. Chem Geol 202 (1?2):59?79

4. Ayllon F (2003) Mineral, fluid and thermal evolution in veins from late orogenic coal basins of the Cantabrian Zone (Variscan, NW Spain). Dissertation am Geologisch-Paläontologischen Institut der Universität Heidelberg. URL: http://www.ub.uni-heidelberg.de/archiv/3391

5. Baadsgaard H, Chaplin C, Griffin WL (1986) Geochronology of the Gloserneia pegmatite, Froland, Southern Norway. Nor Geol Tidsskr 64:111?119

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